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description Publicationkeyboard_double_arrow_right Article , Journal , Research 2015 GermanyPublisher:IOP Publishing Dieter Gerten; Sibyll Schaphoff; Sebastian Ostberg; Wolfgang Lucht; Wolfgang Lucht;Human land use and anthropogenic climate change (CC) are placing mounting pressure on natural ecosystems worldwide, with impacts on biodiversity, water resources, nutrient and carbon cycles. Here, we present a quantitative macro-scale comparative analysis of the separate and joint dual impacts of land use and land cover change (LULCC) and CC on the terrestrial biosphere during the last ca. 300 years, based on simulations with a dynamic global vegetation model and an aggregated metric of simultaneous biogeochemical, hydrological and vegetation-structural shifts. We find that by the beginning of the 21st century LULCC and CC have jointly caused major shifts on more than 90% of all areas now cultivated, corresponding to 26% of the land area. CC has exposed another 26% of natural ecosystems to moderate or major shifts. Within three centuries, the impact of LULCC on landscapes has increased 13-fold. Within just one century, CC effects have caught up with LULCC effects.
Publication Database... arrow_drop_down Publikationsserver der Humboldt-Universität zu BerlinArticle . 2015 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu Berlinadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 58 citations 58 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!
visibility 69visibility views 69 download downloads 51 Powered bymore_vert Publication Database... arrow_drop_down Publikationsserver der Humboldt-Universität zu BerlinArticle . 2015 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu Berlinadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1088/1748-9326/10/4/044011&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Journal , Research 2015 GermanyPublisher:IOP Publishing Dieter Gerten; Sibyll Schaphoff; Sebastian Ostberg; Wolfgang Lucht; Wolfgang Lucht;Human land use and anthropogenic climate change (CC) are placing mounting pressure on natural ecosystems worldwide, with impacts on biodiversity, water resources, nutrient and carbon cycles. Here, we present a quantitative macro-scale comparative analysis of the separate and joint dual impacts of land use and land cover change (LULCC) and CC on the terrestrial biosphere during the last ca. 300 years, based on simulations with a dynamic global vegetation model and an aggregated metric of simultaneous biogeochemical, hydrological and vegetation-structural shifts. We find that by the beginning of the 21st century LULCC and CC have jointly caused major shifts on more than 90% of all areas now cultivated, corresponding to 26% of the land area. CC has exposed another 26% of natural ecosystems to moderate or major shifts. Within three centuries, the impact of LULCC on landscapes has increased 13-fold. Within just one century, CC effects have caught up with LULCC effects.
Publication Database... arrow_drop_down Publikationsserver der Humboldt-Universität zu BerlinArticle . 2015 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu Berlinadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1088/1748-9326/10/4/044011&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 58 citations 58 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!
visibility 69visibility views 69 download downloads 51 Powered bymore_vert Publication Database... arrow_drop_down Publikationsserver der Humboldt-Universität zu BerlinArticle . 2015 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu Berlinadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1088/1748-9326/10/4/044011&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type , Journal 2017 France, United States, France, United Kingdom, United States, Germany, France, Sweden, Netherlands, Spain, Netherlands, United Kingdom, United States, NetherlandsPublisher:Copernicus GmbH Funded by:EC | SIM4NEXUS, EC | CD-LINKS, NWO | Multi-scale and self-cons... +6 projectsEC| SIM4NEXUS ,EC| CD-LINKS ,NWO| Multi-scale and self-consistent observations of recent sea level change ,EC| IMBALANCE-P ,EC| GREEN-WIN ,NSF| Collaborative Research: EaSM2--Wildfires and Regional Climate Variability - Mechanisms, Modeling, and Prediction ,EC| RISES-AM- ,EC| CRESCENDO ,EC| HELIXK. Frieler; S. Lange; F. Piontek; C. P. O. Reyer; J. Schewe; L. Warszawski; F. Zhao; L. Chini; S. Denvil; K. Emanuel; T. Geiger; K. Halladay; G. Hurtt; M. Mengel; D. Murakami; S. Ostberg; S. Ostberg; A. Popp; R. Riva; R. Riva; M. Stevanovic; T. Suzuki; J. Volkholz; E. Burke; P. Ciais; K. Ebi; T. D. Eddy; T. D. Eddy; J. Elliott; J. Elliott; E. Galbraith; E. Galbraith; S. N. Gosling; F. Hattermann; T. Hickler; J. Hinkel; J. Hinkel; C. Hof; V. Huber; J. Jägermeyr; V. Krysanova; R. Marcé; H. Müller Schmied; H. Müller Schmied; I. Mouratiadou; I. Mouratiadou; D. Pierson; D. P. Tittensor; D. P. Tittensor; R. Vautard; M. van Vliet; M. F. Biber; R. A. Betts; R. A. Betts; B. L. Bodirsky; D. Deryng; D. Deryng; S. Frolking; C. D. Jones; H. K. Lotze; H. Lotze-Campen; H. Lotze-Campen; R. Sahajpal; K. Thonicke; H. Tian; H. Tian; Y. Yamagata;handle: 1721.1/119493
Abstract. In Paris, France, December 2015, the Conference of the Parties (COP) to the United Nations Framework Convention on Climate Change (UNFCCC) invited the Intergovernmental Panel on Climate Change (IPCC) to provide a special report in 2018 on the impacts of global warming of 1.5 °C above pre-industrial levels and related global greenhouse gas emission pathways. In Nairobi, Kenya, April 2016, the IPCC panel accepted the invitation. Here we describe the response devised within the Inter-Sectoral Impact Model Intercomparison Project (ISIMIP) to provide tailored, cross-sectorally consistent impact projections to broaden the scientific basis for the report. The simulation protocol is designed to allow for (1) separation of the impacts of historical warming starting from pre-industrial conditions from impacts of other drivers such as historical land-use changes (based on pre-industrial and historical impact model simulations); (2) quantification of the impacts of additional warming up to 1.5 °C, including a potential overshoot and long-term impacts up to 2299, and comparison to higher levels of global mean temperature change (based on the low-emissions Representative Concentration Pathway RCP2.6 and a no-mitigation pathway RCP6.0) with socio-economic conditions fixed at 2005 levels; and (3) assessment of the climate effects based on the same climate scenarios while accounting for simultaneous changes in socio-economic conditions following the middle-of-the-road Shared Socioeconomic Pathway (SSP2, Fricko et al., 2016) and in particular differential bioenergy requirements associated with the transformation of the energy system to comply with RCP2.6 compared to RCP6.0. With the aim of providing the scientific basis for an aggregation of impacts across sectors and analysis of cross-sectoral interactions that may dampen or amplify sectoral impacts, the protocol is designed to facilitate consistent impact projections from a range of impact models across different sectors (global and regional hydrology, lakes, global crops, global vegetation, regional forests, global and regional marine ecosystems and fisheries, global and regional coastal infrastructure, energy supply and demand, temperature-related mortality, and global terrestrial biodiversity).
Nottingham Research ... arrow_drop_down University of New Hampshire: Scholars RepositoryArticle . 2017License: CC BYFull-Text: https://scholars.unh.edu/ersc/203Data sources: Bielefeld Academic Search Engine (BASE)DSpace@MIT (Massachusetts Institute of Technology)Article . 2017License: CC BYFull-Text: https://doi.org/10.5194/gmd-10-4321-2017Data sources: Bielefeld Academic Search Engine (BASE)Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2017License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2017Full-Text: https://hal.science/hal-02922298Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2017Full-Text: https://hal.science/hal-02922298Data sources: Bielefeld Academic Search Engine (BASE)Geoscientific Model DevelopmentArticle . 2017Data sources: DANS (Data Archiving and Networked Services)Geoscientific Model DevelopmentArticle . 2017Data sources: DANS (Data Archiving and Networked Services)Recolector de Ciencia Abierta, RECOLECTAArticle . 2017License: CC BYData sources: Recolector de Ciencia Abierta, RECOLECTADiposit Digital de Documents de la UABArticle . 2017License: CC BYData sources: Diposit Digital de Documents de la UABFachrepositorium LebenswissenschaftenArticle . 2017License: CC BYData sources: Fachrepositorium LebenswissenschaftenPublikationer från Uppsala UniversitetArticle . 2017Data sources: Publikationer från Uppsala UniversitetWageningen Staff PublicationsArticle . 2017License: CC BYData sources: Wageningen Staff PublicationsDigitala Vetenskapliga Arkivet - Academic Archive On-lineArticle . 2017 . Peer-reviewedGeoscientific Model DevelopmentArticle . 2017 . Peer-reviewedData sources: European Union Open Data PortalDelft University of Technology: Institutional RepositoryArticle . 2017Data sources: Bielefeld Academic Search Engine (BASE)Knowledge@UChicago (University of Chicago)Article . 2024Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 467 citations 467 popularity Top 0.1% influence Top 1% impulse Top 0.1% Powered by BIP!
visibility 6visibility views 6 download downloads 18 Powered bymore_vert Nottingham Research ... arrow_drop_down University of New Hampshire: Scholars RepositoryArticle . 2017License: CC BYFull-Text: https://scholars.unh.edu/ersc/203Data sources: Bielefeld Academic Search Engine (BASE)DSpace@MIT (Massachusetts Institute of Technology)Article . 2017License: CC BYFull-Text: https://doi.org/10.5194/gmd-10-4321-2017Data sources: Bielefeld Academic Search Engine (BASE)Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2017License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2017Full-Text: https://hal.science/hal-02922298Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2017Full-Text: https://hal.science/hal-02922298Data sources: Bielefeld Academic Search Engine (BASE)Geoscientific Model DevelopmentArticle . 2017Data sources: DANS (Data Archiving and Networked Services)Geoscientific Model DevelopmentArticle . 2017Data sources: DANS (Data Archiving and Networked Services)Recolector de Ciencia Abierta, RECOLECTAArticle . 2017License: CC BYData sources: Recolector de Ciencia Abierta, RECOLECTADiposit Digital de Documents de la UABArticle . 2017License: CC BYData sources: Diposit Digital de Documents de la UABFachrepositorium LebenswissenschaftenArticle . 2017License: CC BYData sources: Fachrepositorium LebenswissenschaftenPublikationer från Uppsala UniversitetArticle . 2017Data sources: Publikationer från Uppsala UniversitetWageningen Staff PublicationsArticle . 2017License: CC BYData sources: Wageningen Staff PublicationsDigitala Vetenskapliga Arkivet - Academic Archive On-lineArticle . 2017 . Peer-reviewedGeoscientific Model DevelopmentArticle . 2017 . Peer-reviewedData sources: European Union Open Data PortalDelft University of Technology: Institutional RepositoryArticle . 2017Data sources: Bielefeld Academic Search Engine (BASE)Knowledge@UChicago (University of Chicago)Article . 2024Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/gmd-10-4321-2017&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type , Journal 2017 France, United States, France, United Kingdom, United States, Germany, France, Sweden, Netherlands, Spain, Netherlands, United Kingdom, United States, NetherlandsPublisher:Copernicus GmbH Funded by:EC | SIM4NEXUS, EC | CD-LINKS, NWO | Multi-scale and self-cons... +6 projectsEC| SIM4NEXUS ,EC| CD-LINKS ,NWO| Multi-scale and self-consistent observations of recent sea level change ,EC| IMBALANCE-P ,EC| GREEN-WIN ,NSF| Collaborative Research: EaSM2--Wildfires and Regional Climate Variability - Mechanisms, Modeling, and Prediction ,EC| RISES-AM- ,EC| CRESCENDO ,EC| HELIXK. Frieler; S. Lange; F. Piontek; C. P. O. Reyer; J. Schewe; L. Warszawski; F. Zhao; L. Chini; S. Denvil; K. Emanuel; T. Geiger; K. Halladay; G. Hurtt; M. Mengel; D. Murakami; S. Ostberg; S. Ostberg; A. Popp; R. Riva; R. Riva; M. Stevanovic; T. Suzuki; J. Volkholz; E. Burke; P. Ciais; K. Ebi; T. D. Eddy; T. D. Eddy; J. Elliott; J. Elliott; E. Galbraith; E. Galbraith; S. N. Gosling; F. Hattermann; T. Hickler; J. Hinkel; J. Hinkel; C. Hof; V. Huber; J. Jägermeyr; V. Krysanova; R. Marcé; H. Müller Schmied; H. Müller Schmied; I. Mouratiadou; I. Mouratiadou; D. Pierson; D. P. Tittensor; D. P. Tittensor; R. Vautard; M. van Vliet; M. F. Biber; R. A. Betts; R. A. Betts; B. L. Bodirsky; D. Deryng; D. Deryng; S. Frolking; C. D. Jones; H. K. Lotze; H. Lotze-Campen; H. Lotze-Campen; R. Sahajpal; K. Thonicke; H. Tian; H. Tian; Y. Yamagata;handle: 1721.1/119493
Abstract. In Paris, France, December 2015, the Conference of the Parties (COP) to the United Nations Framework Convention on Climate Change (UNFCCC) invited the Intergovernmental Panel on Climate Change (IPCC) to provide a special report in 2018 on the impacts of global warming of 1.5 °C above pre-industrial levels and related global greenhouse gas emission pathways. In Nairobi, Kenya, April 2016, the IPCC panel accepted the invitation. Here we describe the response devised within the Inter-Sectoral Impact Model Intercomparison Project (ISIMIP) to provide tailored, cross-sectorally consistent impact projections to broaden the scientific basis for the report. The simulation protocol is designed to allow for (1) separation of the impacts of historical warming starting from pre-industrial conditions from impacts of other drivers such as historical land-use changes (based on pre-industrial and historical impact model simulations); (2) quantification of the impacts of additional warming up to 1.5 °C, including a potential overshoot and long-term impacts up to 2299, and comparison to higher levels of global mean temperature change (based on the low-emissions Representative Concentration Pathway RCP2.6 and a no-mitigation pathway RCP6.0) with socio-economic conditions fixed at 2005 levels; and (3) assessment of the climate effects based on the same climate scenarios while accounting for simultaneous changes in socio-economic conditions following the middle-of-the-road Shared Socioeconomic Pathway (SSP2, Fricko et al., 2016) and in particular differential bioenergy requirements associated with the transformation of the energy system to comply with RCP2.6 compared to RCP6.0. With the aim of providing the scientific basis for an aggregation of impacts across sectors and analysis of cross-sectoral interactions that may dampen or amplify sectoral impacts, the protocol is designed to facilitate consistent impact projections from a range of impact models across different sectors (global and regional hydrology, lakes, global crops, global vegetation, regional forests, global and regional marine ecosystems and fisheries, global and regional coastal infrastructure, energy supply and demand, temperature-related mortality, and global terrestrial biodiversity).
Nottingham Research ... arrow_drop_down University of New Hampshire: Scholars RepositoryArticle . 2017License: CC BYFull-Text: https://scholars.unh.edu/ersc/203Data sources: Bielefeld Academic Search Engine (BASE)DSpace@MIT (Massachusetts Institute of Technology)Article . 2017License: CC BYFull-Text: https://doi.org/10.5194/gmd-10-4321-2017Data sources: Bielefeld Academic Search Engine (BASE)Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2017License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2017Full-Text: https://hal.science/hal-02922298Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2017Full-Text: https://hal.science/hal-02922298Data sources: Bielefeld Academic Search Engine (BASE)Geoscientific Model DevelopmentArticle . 2017Data sources: DANS (Data Archiving and Networked Services)Geoscientific Model DevelopmentArticle . 2017Data sources: DANS (Data Archiving and Networked Services)Recolector de Ciencia Abierta, RECOLECTAArticle . 2017License: CC BYData sources: Recolector de Ciencia Abierta, RECOLECTADiposit Digital de Documents de la UABArticle . 2017License: CC BYData sources: Diposit Digital de Documents de la UABFachrepositorium LebenswissenschaftenArticle . 2017License: CC BYData sources: Fachrepositorium LebenswissenschaftenPublikationer från Uppsala UniversitetArticle . 2017Data sources: Publikationer från Uppsala UniversitetWageningen Staff PublicationsArticle . 2017License: CC BYData sources: Wageningen Staff PublicationsDigitala Vetenskapliga Arkivet - Academic Archive On-lineArticle . 2017 . Peer-reviewedGeoscientific Model DevelopmentArticle . 2017 . Peer-reviewedData sources: European Union Open Data PortalDelft University of Technology: Institutional RepositoryArticle . 2017Data sources: Bielefeld Academic Search Engine (BASE)Knowledge@UChicago (University of Chicago)Article . 2024Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/gmd-10-4321-2017&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 467 citations 467 popularity Top 0.1% influence Top 1% impulse Top 0.1% Powered by BIP!
visibility 6visibility views 6 download downloads 18 Powered bymore_vert Nottingham Research ... arrow_drop_down University of New Hampshire: Scholars RepositoryArticle . 2017License: CC BYFull-Text: https://scholars.unh.edu/ersc/203Data sources: Bielefeld Academic Search Engine (BASE)DSpace@MIT (Massachusetts Institute of Technology)Article . 2017License: CC BYFull-Text: https://doi.org/10.5194/gmd-10-4321-2017Data sources: Bielefeld Academic Search Engine (BASE)Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2017License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2017Full-Text: https://hal.science/hal-02922298Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2017Full-Text: https://hal.science/hal-02922298Data sources: Bielefeld Academic Search Engine (BASE)Geoscientific Model DevelopmentArticle . 2017Data sources: DANS (Data Archiving and Networked Services)Geoscientific Model DevelopmentArticle . 2017Data sources: DANS (Data Archiving and Networked Services)Recolector de Ciencia Abierta, RECOLECTAArticle . 2017License: CC BYData sources: Recolector de Ciencia Abierta, RECOLECTADiposit Digital de Documents de la UABArticle . 2017License: CC BYData sources: Diposit Digital de Documents de la UABFachrepositorium LebenswissenschaftenArticle . 2017License: CC BYData sources: Fachrepositorium LebenswissenschaftenPublikationer från Uppsala UniversitetArticle . 2017Data sources: Publikationer från Uppsala UniversitetWageningen Staff PublicationsArticle . 2017License: CC BYData sources: Wageningen Staff PublicationsDigitala Vetenskapliga Arkivet - Academic Archive On-lineArticle . 2017 . Peer-reviewedGeoscientific Model DevelopmentArticle . 2017 . Peer-reviewedData sources: European Union Open Data PortalDelft University of Technology: Institutional RepositoryArticle . 2017Data sources: Bielefeld Academic Search Engine (BASE)Knowledge@UChicago (University of Chicago)Article . 2024Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/gmd-10-4321-2017&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Conference object , Other literature type , Journal 2017 France, France, France, France, France, France, Germany, FrancePublisher:IOP Publishing Funded by:EC | IMBALANCE-P, NSF | Collaborative Research: E..., EC | HELIXEC| IMBALANCE-P ,NSF| Collaborative Research: EaSM2--Wildfires and Regional Climate Variability - Mechanisms, Modeling, and Prediction ,EC| HELIXAuthors: Sibyll Schaphoff; Christopher P. O. Reyer; Frédéric Chevallier; Jörg Steinkamp; +29 AuthorsSibyll Schaphoff; Christopher P. O. Reyer; Frédéric Chevallier; Jörg Steinkamp; Jia Yang; Rashid Rafique; Ghassem R. Asrar; Ning Zeng; Kazuya Nishina; Akihiko Ito; Shushi Peng; Fang Zhao; Shufen Pan; Sebastian Ostberg; Sebastian Ostberg; Jinfeng Chang; Jinfeng Chang; Louis François; Shilong Piao; Katja Frieler; Guy Munhoven; Marie Dury; Thomas Hickler; Philippe Ciais; Xuhui Wang; Xuhui Wang; Alexandra-Jane Henrot; Hanqin Tian; Christrian Rödenbeck; Anselmo Garcia Cantu Ros; Richard Betts; Nicolas Viovy; Catherine Morfopoulos;Le but de cette étude est d'évaluer les huit modèles de biome ISIMIP2a par rapport à des estimations indépendantes des flux nets de carbone à long terme (c'est-à-dire la productivité nette du biome, NBP) sur les écosystèmes terrestres au cours des quatre dernières décennies (1971–2010). Nous évaluons le NBP mondial modélisé par rapport à 1) le puits terrestre résiduel mondial (RLS) mis à jour plus les émissions liées à l'utilisation des terres (ELUC) du Global Carbon Project (GCP), présenté comme R + L dans cette étude par Le Quéré et al (2015), et 2) les flux de CO2 terrestre provenant de deux systèmes d'inversion atmosphérique : Jena CarboScope s81_v3.8 et CAMS v15r2, appelés FJena et FCAMS respectivement. L'ensemble de modèles - moyenne NBP (qui comprend sept modèles avec changement d'affectation des terres) est plus élevé que mais dans l'incertitude de R + L, tandis que la tendance NBP positive simulée au cours des 30 dernières années est inférieure à celle de R + L et des deux systèmes d'inversion. Les modèles de biome ISIMIP2a capturent bien la variation interannuelle des flux nets mondiaux de carbone des écosystèmes terrestres. La NBP tropicale représente 31 ± 17 % de la NBP totale mondiale au cours des dernières décennies, et la variation d'une année à l'autre de la NBP tropicale contribue pour l'essentiel à la variation interannuelle de la NBP mondiale. Selon les modèles, l'augmentation de la productivité primaire nette (NPP) a été la principale cause de l'augmentation générale de la NBP. Des anomalies NBP globales significatives à partir de la moyenne à long terme entre les deux phases des événements El Niño Southern Oscillation (ENSO) sont simulées par tous les modèles (p < 0,05), ce qui est cohérent avec l'estimation R + L (p = 0,06), également principalement attribuée à des anomalies NPP, plutôt qu'à des changements dans la respiration hétérotrophique (Rh). Les anomalies mondiales de la centrale nucléaire et de la centrale nucléaire nucléaire pendant les événements ENSO sont dominées par leurs anomalies dans les régions tropicales touchées par la variabilité du climat tropical. Les régressions multiples entre les variations interannuelles de R + L, FJena et FCAMS et les variations du climat tropical révèlent une réponse négative significative des flux nets mondiaux de carbone des écosystèmes terrestres à la variation de la température annuelle moyenne tropicale, et une réponse non significative à la variation des précipitations annuelles tropicales. Selon les modèles, les précipitations tropicales sont un facteur plus important, ce qui suggère que certains modèles ne saisissent pas correctement les rôles des précipitations et des changements de température. El propósito de este estudio es evaluar los ocho modelos de bioma ISIMIP2a contra estimaciones independientes de flujos netos de carbono a largo plazo (es decir, Productividad Neta del Bioma, NBP) sobre ecosistemas terrestres durante las últimas cuatro décadas (1971–2010). Evaluamos el NBP global modelado contra 1) el sumidero de tierra residual (RLS) global actualizado más las emisiones de uso de la tierra (ELUC) del Proyecto Global de Carbono (GCP), presentado como R + L en este estudio por Le Quéré et al (2015), y 2) los flujos de CO2 terrestre de dos sistemas de inversión atmosférica: Jena CarboScope s81_v3.8 y CAMS v15r2, denominados FJena y FCAMS respectivamente. La media del conjunto de modelos NBP (que incluye siete modelos con cambio de uso de la tierra) es mayor que, pero dentro de la incertidumbre de R + L, mientras que la tendencia positiva simulada de NBP en los últimos 30 años es menor que la de R + L y de los dos sistemas de inversión. Los modelos de bioma ISIMIP2a capturan bien la variación interanual de los flujos netos globales de carbono del ecosistema terrestre. El NBP tropical representa el 31 ± 17% del NBP total global durante las últimas décadas, y la variación interanual del NBP tropical contribuye con la mayor parte de la variación interanual del NBP global. Según los modelos, el aumento de la productividad primaria neta (PPN) fue la causa principal del aumento general de la PNB. Todos los modelos simulan anomalías de NBP globales significativas de la media a largo plazo entre las dos fases de los eventos de El Niño Oscilación del Sur (Enos) (p < 0.05), lo cual es consistente con la estimación de R + L (p = 0.06), también atribuida principalmente a anomalías de NPP, más que a cambios en la respiración heterótrofa (Rh). Las anomalías globales de NPP y NBP durante los eventos Enos están dominadas por sus anomalías en las regiones tropicales afectadas por la variabilidad del clima tropical. Las múltiples regresiones entre las variaciones interanuales de R + L, FJena y FCAMS y las variaciones del clima tropical revelan una respuesta negativa significativa de los flujos netos globales de carbono del ecosistema terrestre a la variación de la temperatura media anual tropical, y una respuesta no significativa a la variación de la precipitación anual tropical. Según los modelos, la precipitación tropical es un impulsor más importante, lo que sugiere que algunos modelos no capturan adecuadamente los roles de la precipitación y los cambios de temperatura. The purpose of this study is to evaluate the eight ISIMIP2a biome models against independent estimates of long-term net carbon fluxes (i.e. Net Biome Productivity, NBP) over terrestrial ecosystems for the recent four decades (1971–2010). We evaluate modeled global NBP against 1) the updated global residual land sink (RLS) plus land use emissions (ELUC) from the Global Carbon Project (GCP), presented as R + L in this study by Le Quéré et al (2015), and 2) the land CO2 fluxes from two atmospheric inversion systems: Jena CarboScope s81_v3.8 and CAMS v15r2, referred to as FJena and FCAMS respectively. The model ensemble-mean NBP (that includes seven models with land-use change) is higher than but within the uncertainty of R + L, while the simulated positive NBP trend over the last 30 yr is lower than that from R + L and from the two inversion systems. ISIMIP2a biome models well capture the interannual variation of global net terrestrial ecosystem carbon fluxes. Tropical NBP represents 31 ± 17% of global total NBP during the past decades, and the year-to-year variation of tropical NBP contributes most of the interannual variation of global NBP. According to the models, increasing Net Primary Productivity (NPP) was the main cause for the generally increasing NBP. Significant global NBP anomalies from the long-term mean between the two phases of El Niño Southern Oscillation (ENSO) events are simulated by all models (p < 0.05), which is consistent with the R + L estimate (p = 0.06), also mainly attributed to NPP anomalies, rather than to changes in heterotrophic respiration (Rh). The global NPP and NBP anomalies during ENSO events are dominated by their anomalies in tropical regions impacted by tropical climate variability. Multiple regressions between R + L, FJena and FCAMS interannual variations and tropical climate variations reveal a significant negative response of global net terrestrial ecosystem carbon fluxes to tropical mean annual temperature variation, and a non-significant response to tropical annual precipitation variation. According to the models, tropical precipitation is a more important driver, suggesting that some models do not capture the roles of precipitation and temperature changes adequately. الغرض من هذه الدراسة هو تقييم نماذج المناطق الأحيائية الثمانية ISIMIP2a مقابل التقديرات المستقلة لصافي تدفقات الكربون طويلة الأجل (أي صافي إنتاجية المناطق الأحيائية) على النظم الإيكولوجية الأرضية على مدى العقود الأربعة الأخيرة (1971–2010). نقوم بتقييم خطة العمل الوطنية العالمية المنمذجة مقابل 1) بالوعة الأراضي المتبقية العالمية المحدثة بالإضافة إلى انبعاثات استخدام الأراضي (ELUC) من مشروع الكربون العالمي (GCP)، والتي تم تقديمها على أنها R + L في هذه الدراسة من قبل Le Quéré et al (2015)، و 2) تدفقات ثاني أكسيد الكربون الأرضية من نظامين لعكس الغلاف الجوي: Jena CarboScope s81_v3.8 و CAMS v15r2، المشار إليها باسم FJena و FCAMS على التوالي. إن مجموعة النماذج - تعني NBP (التي تتضمن سبعة نماذج مع تغيير استخدام الأراضي) أعلى من ولكن ضمن عدم اليقين من R + L، في حين أن اتجاه NBP الإيجابي المحاكي على مدار الثلاثين عامًا الماضية أقل من ذلك من R + L ومن نظامي الانعكاس. تلتقط نماذج المناطق الأحيائية ISIMIP2a بشكل جيد التباين السنوي لتدفقات الكربون الصافية للنظام الإيكولوجي الأرضي العالمي. يمثل الناتج القومي الاستوائي 31 ± 17 ٪ من إجمالي الناتج القومي العالمي خلال العقود الماضية، ويساهم التباين من سنة إلى أخرى في الناتج القومي الاستوائي في معظم التباين السنوي في الناتج القومي العالمي. وفقًا للنماذج، كانت زيادة صافي الإنتاجية الأولية هي السبب الرئيسي لزيادة صافي الإنتاجية الأولية بشكل عام. تتم محاكاة حالات الشذوذ العالمية الكبيرة من المتوسط طويل الأجل بين مرحلتي أحداث التذبذب الجنوبي لظاهرة النينيو (ENSO) من خلال جميع النماذج (P < 0.05)، وهو ما يتوافق مع تقدير R + L (P = 0.06)، والذي يعزى أيضًا بشكل أساسي إلى حالات الشذوذ في NPP، بدلاً من التغيرات في التنفس غيري التغذية (Rh). تهيمن الشذوذات العالمية لمحطات الطاقة النووية ومحطات الطاقة الوطنية خلال أحداث ENSO على شذوذاتها في المناطق المدارية المتأثرة بتقلب المناخ المداري. تكشف الانحدارات المتعددة بين الاختلافات السنوية بين R + L و FJENA و FCAMS والتغيرات المناخية المدارية عن استجابة سلبية كبيرة لصافي تدفقات الكربون في النظام الإيكولوجي الأرضي العالمي لمتوسط التغير السنوي في درجة الحرارة المدارية، واستجابة غير كبيرة لتغير هطول الأمطار السنوي المداري. وفقًا للنماذج، يعد هطول الأمطار الاستوائية محركًا أكثر أهمية، مما يشير إلى أن بعض النماذج لا تلتقط أدوار هطول الأمطار وتغيرات درجة الحرارة بشكل كافٍ.
Hyper Article en Lig... arrow_drop_down École Polytechnique, Université Paris-Saclay: HALArticle . 2017Full-Text: https://hal.science/hal-01828297Data sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2017Full-Text: https://hal.science/hal-01828297Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2017Full-Text: https://hal.science/hal-01828297Data sources: Bielefeld Academic Search Engine (BASE)Fachrepositorium LebenswissenschaftenArticle . 2017License: CC BYData sources: Fachrepositorium Lebenswissenschaftenhttp://dx.doi.org/https://iops...Other literature typeData sources: European Union Open Data Portaladd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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more_vert Hyper Article en Lig... arrow_drop_down École Polytechnique, Université Paris-Saclay: HALArticle . 2017Full-Text: https://hal.science/hal-01828297Data sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2017Full-Text: https://hal.science/hal-01828297Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2017Full-Text: https://hal.science/hal-01828297Data sources: Bielefeld Academic Search Engine (BASE)Fachrepositorium LebenswissenschaftenArticle . 2017License: CC BYData sources: Fachrepositorium Lebenswissenschaftenhttp://dx.doi.org/https://iops...Other literature typeData sources: European Union Open Data Portaladd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Conference object , Other literature type , Journal 2017 France, France, France, France, France, France, Germany, FrancePublisher:IOP Publishing Funded by:EC | IMBALANCE-P, NSF | Collaborative Research: E..., EC | HELIXEC| IMBALANCE-P ,NSF| Collaborative Research: EaSM2--Wildfires and Regional Climate Variability - Mechanisms, Modeling, and Prediction ,EC| HELIXAuthors: Sibyll Schaphoff; Christopher P. O. Reyer; Frédéric Chevallier; Jörg Steinkamp; +29 AuthorsSibyll Schaphoff; Christopher P. O. Reyer; Frédéric Chevallier; Jörg Steinkamp; Jia Yang; Rashid Rafique; Ghassem R. Asrar; Ning Zeng; Kazuya Nishina; Akihiko Ito; Shushi Peng; Fang Zhao; Shufen Pan; Sebastian Ostberg; Sebastian Ostberg; Jinfeng Chang; Jinfeng Chang; Louis François; Shilong Piao; Katja Frieler; Guy Munhoven; Marie Dury; Thomas Hickler; Philippe Ciais; Xuhui Wang; Xuhui Wang; Alexandra-Jane Henrot; Hanqin Tian; Christrian Rödenbeck; Anselmo Garcia Cantu Ros; Richard Betts; Nicolas Viovy; Catherine Morfopoulos;Le but de cette étude est d'évaluer les huit modèles de biome ISIMIP2a par rapport à des estimations indépendantes des flux nets de carbone à long terme (c'est-à-dire la productivité nette du biome, NBP) sur les écosystèmes terrestres au cours des quatre dernières décennies (1971–2010). Nous évaluons le NBP mondial modélisé par rapport à 1) le puits terrestre résiduel mondial (RLS) mis à jour plus les émissions liées à l'utilisation des terres (ELUC) du Global Carbon Project (GCP), présenté comme R + L dans cette étude par Le Quéré et al (2015), et 2) les flux de CO2 terrestre provenant de deux systèmes d'inversion atmosphérique : Jena CarboScope s81_v3.8 et CAMS v15r2, appelés FJena et FCAMS respectivement. L'ensemble de modèles - moyenne NBP (qui comprend sept modèles avec changement d'affectation des terres) est plus élevé que mais dans l'incertitude de R + L, tandis que la tendance NBP positive simulée au cours des 30 dernières années est inférieure à celle de R + L et des deux systèmes d'inversion. Les modèles de biome ISIMIP2a capturent bien la variation interannuelle des flux nets mondiaux de carbone des écosystèmes terrestres. La NBP tropicale représente 31 ± 17 % de la NBP totale mondiale au cours des dernières décennies, et la variation d'une année à l'autre de la NBP tropicale contribue pour l'essentiel à la variation interannuelle de la NBP mondiale. Selon les modèles, l'augmentation de la productivité primaire nette (NPP) a été la principale cause de l'augmentation générale de la NBP. Des anomalies NBP globales significatives à partir de la moyenne à long terme entre les deux phases des événements El Niño Southern Oscillation (ENSO) sont simulées par tous les modèles (p < 0,05), ce qui est cohérent avec l'estimation R + L (p = 0,06), également principalement attribuée à des anomalies NPP, plutôt qu'à des changements dans la respiration hétérotrophique (Rh). Les anomalies mondiales de la centrale nucléaire et de la centrale nucléaire nucléaire pendant les événements ENSO sont dominées par leurs anomalies dans les régions tropicales touchées par la variabilité du climat tropical. Les régressions multiples entre les variations interannuelles de R + L, FJena et FCAMS et les variations du climat tropical révèlent une réponse négative significative des flux nets mondiaux de carbone des écosystèmes terrestres à la variation de la température annuelle moyenne tropicale, et une réponse non significative à la variation des précipitations annuelles tropicales. Selon les modèles, les précipitations tropicales sont un facteur plus important, ce qui suggère que certains modèles ne saisissent pas correctement les rôles des précipitations et des changements de température. El propósito de este estudio es evaluar los ocho modelos de bioma ISIMIP2a contra estimaciones independientes de flujos netos de carbono a largo plazo (es decir, Productividad Neta del Bioma, NBP) sobre ecosistemas terrestres durante las últimas cuatro décadas (1971–2010). Evaluamos el NBP global modelado contra 1) el sumidero de tierra residual (RLS) global actualizado más las emisiones de uso de la tierra (ELUC) del Proyecto Global de Carbono (GCP), presentado como R + L en este estudio por Le Quéré et al (2015), y 2) los flujos de CO2 terrestre de dos sistemas de inversión atmosférica: Jena CarboScope s81_v3.8 y CAMS v15r2, denominados FJena y FCAMS respectivamente. La media del conjunto de modelos NBP (que incluye siete modelos con cambio de uso de la tierra) es mayor que, pero dentro de la incertidumbre de R + L, mientras que la tendencia positiva simulada de NBP en los últimos 30 años es menor que la de R + L y de los dos sistemas de inversión. Los modelos de bioma ISIMIP2a capturan bien la variación interanual de los flujos netos globales de carbono del ecosistema terrestre. El NBP tropical representa el 31 ± 17% del NBP total global durante las últimas décadas, y la variación interanual del NBP tropical contribuye con la mayor parte de la variación interanual del NBP global. Según los modelos, el aumento de la productividad primaria neta (PPN) fue la causa principal del aumento general de la PNB. Todos los modelos simulan anomalías de NBP globales significativas de la media a largo plazo entre las dos fases de los eventos de El Niño Oscilación del Sur (Enos) (p < 0.05), lo cual es consistente con la estimación de R + L (p = 0.06), también atribuida principalmente a anomalías de NPP, más que a cambios en la respiración heterótrofa (Rh). Las anomalías globales de NPP y NBP durante los eventos Enos están dominadas por sus anomalías en las regiones tropicales afectadas por la variabilidad del clima tropical. Las múltiples regresiones entre las variaciones interanuales de R + L, FJena y FCAMS y las variaciones del clima tropical revelan una respuesta negativa significativa de los flujos netos globales de carbono del ecosistema terrestre a la variación de la temperatura media anual tropical, y una respuesta no significativa a la variación de la precipitación anual tropical. Según los modelos, la precipitación tropical es un impulsor más importante, lo que sugiere que algunos modelos no capturan adecuadamente los roles de la precipitación y los cambios de temperatura. The purpose of this study is to evaluate the eight ISIMIP2a biome models against independent estimates of long-term net carbon fluxes (i.e. Net Biome Productivity, NBP) over terrestrial ecosystems for the recent four decades (1971–2010). We evaluate modeled global NBP against 1) the updated global residual land sink (RLS) plus land use emissions (ELUC) from the Global Carbon Project (GCP), presented as R + L in this study by Le Quéré et al (2015), and 2) the land CO2 fluxes from two atmospheric inversion systems: Jena CarboScope s81_v3.8 and CAMS v15r2, referred to as FJena and FCAMS respectively. The model ensemble-mean NBP (that includes seven models with land-use change) is higher than but within the uncertainty of R + L, while the simulated positive NBP trend over the last 30 yr is lower than that from R + L and from the two inversion systems. ISIMIP2a biome models well capture the interannual variation of global net terrestrial ecosystem carbon fluxes. Tropical NBP represents 31 ± 17% of global total NBP during the past decades, and the year-to-year variation of tropical NBP contributes most of the interannual variation of global NBP. According to the models, increasing Net Primary Productivity (NPP) was the main cause for the generally increasing NBP. Significant global NBP anomalies from the long-term mean between the two phases of El Niño Southern Oscillation (ENSO) events are simulated by all models (p < 0.05), which is consistent with the R + L estimate (p = 0.06), also mainly attributed to NPP anomalies, rather than to changes in heterotrophic respiration (Rh). The global NPP and NBP anomalies during ENSO events are dominated by their anomalies in tropical regions impacted by tropical climate variability. Multiple regressions between R + L, FJena and FCAMS interannual variations and tropical climate variations reveal a significant negative response of global net terrestrial ecosystem carbon fluxes to tropical mean annual temperature variation, and a non-significant response to tropical annual precipitation variation. According to the models, tropical precipitation is a more important driver, suggesting that some models do not capture the roles of precipitation and temperature changes adequately. الغرض من هذه الدراسة هو تقييم نماذج المناطق الأحيائية الثمانية ISIMIP2a مقابل التقديرات المستقلة لصافي تدفقات الكربون طويلة الأجل (أي صافي إنتاجية المناطق الأحيائية) على النظم الإيكولوجية الأرضية على مدى العقود الأربعة الأخيرة (1971–2010). نقوم بتقييم خطة العمل الوطنية العالمية المنمذجة مقابل 1) بالوعة الأراضي المتبقية العالمية المحدثة بالإضافة إلى انبعاثات استخدام الأراضي (ELUC) من مشروع الكربون العالمي (GCP)، والتي تم تقديمها على أنها R + L في هذه الدراسة من قبل Le Quéré et al (2015)، و 2) تدفقات ثاني أكسيد الكربون الأرضية من نظامين لعكس الغلاف الجوي: Jena CarboScope s81_v3.8 و CAMS v15r2، المشار إليها باسم FJena و FCAMS على التوالي. إن مجموعة النماذج - تعني NBP (التي تتضمن سبعة نماذج مع تغيير استخدام الأراضي) أعلى من ولكن ضمن عدم اليقين من R + L، في حين أن اتجاه NBP الإيجابي المحاكي على مدار الثلاثين عامًا الماضية أقل من ذلك من R + L ومن نظامي الانعكاس. تلتقط نماذج المناطق الأحيائية ISIMIP2a بشكل جيد التباين السنوي لتدفقات الكربون الصافية للنظام الإيكولوجي الأرضي العالمي. يمثل الناتج القومي الاستوائي 31 ± 17 ٪ من إجمالي الناتج القومي العالمي خلال العقود الماضية، ويساهم التباين من سنة إلى أخرى في الناتج القومي الاستوائي في معظم التباين السنوي في الناتج القومي العالمي. وفقًا للنماذج، كانت زيادة صافي الإنتاجية الأولية هي السبب الرئيسي لزيادة صافي الإنتاجية الأولية بشكل عام. تتم محاكاة حالات الشذوذ العالمية الكبيرة من المتوسط طويل الأجل بين مرحلتي أحداث التذبذب الجنوبي لظاهرة النينيو (ENSO) من خلال جميع النماذج (P < 0.05)، وهو ما يتوافق مع تقدير R + L (P = 0.06)، والذي يعزى أيضًا بشكل أساسي إلى حالات الشذوذ في NPP، بدلاً من التغيرات في التنفس غيري التغذية (Rh). تهيمن الشذوذات العالمية لمحطات الطاقة النووية ومحطات الطاقة الوطنية خلال أحداث ENSO على شذوذاتها في المناطق المدارية المتأثرة بتقلب المناخ المداري. تكشف الانحدارات المتعددة بين الاختلافات السنوية بين R + L و FJENA و FCAMS والتغيرات المناخية المدارية عن استجابة سلبية كبيرة لصافي تدفقات الكربون في النظام الإيكولوجي الأرضي العالمي لمتوسط التغير السنوي في درجة الحرارة المدارية، واستجابة غير كبيرة لتغير هطول الأمطار السنوي المداري. وفقًا للنماذج، يعد هطول الأمطار الاستوائية محركًا أكثر أهمية، مما يشير إلى أن بعض النماذج لا تلتقط أدوار هطول الأمطار وتغيرات درجة الحرارة بشكل كافٍ.
Hyper Article en Lig... arrow_drop_down École Polytechnique, Université Paris-Saclay: HALArticle . 2017Full-Text: https://hal.science/hal-01828297Data sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2017Full-Text: https://hal.science/hal-01828297Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2017Full-Text: https://hal.science/hal-01828297Data sources: Bielefeld Academic Search Engine (BASE)Fachrepositorium LebenswissenschaftenArticle . 2017License: CC BYData sources: Fachrepositorium Lebenswissenschaftenhttp://dx.doi.org/https://iops...Other literature typeData sources: European Union Open Data Portaladd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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more_vert Hyper Article en Lig... arrow_drop_down École Polytechnique, Université Paris-Saclay: HALArticle . 2017Full-Text: https://hal.science/hal-01828297Data sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2017Full-Text: https://hal.science/hal-01828297Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2017Full-Text: https://hal.science/hal-01828297Data sources: Bielefeld Academic Search Engine (BASE)Fachrepositorium LebenswissenschaftenArticle . 2017License: CC BYData sources: Fachrepositorium Lebenswissenschaftenhttp://dx.doi.org/https://iops...Other literature typeData sources: European Union Open Data Portaladd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2024 Italy, GermanyPublisher:IOP Publishing Lisa Murken; Julia Tomalka; David Abigaba; Antwi-Bosiako Amoah; Joseph Armathé Amougou; Muriel Anaba; Ponraj Arumugam; Eres Awori; Hye-Rin Léa Baek; Till Below; Matti Cartsburg; Abel Chemura; Carla Cronauer; Iulii Didovets; Adefires Worku Gizaw; Stephanie Gleixner; Nele Gloy; Enrico Grams; Lemlem Habtemariam; Anna Hampf; Ylva Hauf; Tim Heckmann; Boubacar Ibrahim; Lennart Jansen; Francis Jarawura; Timothée Kagonbé; Juliane Kaufmann; Priscilla Kephe; Lena Klockemann; Stefan Lange; Rahel Laudien; Stefan Liersch; Naima Lipka; Sophia Lüttringhaus; Sibylla Neer; Oblé Neya; Steffen Noleppa; Sebastian Ostberg; Jonas Pollig; Paula Romanovska; Felicitas Röhrig; Bernhard Schauberger; Roopam Shukla; Lina Staubach; Mesmin Tchindjang; Sabine Undorf; Regina Vetter; Sophie von Loeben; Christoph von Stechow; Katarina von Witzke; Chiara Sophia Weituschat; Michel Wortmann; Amsalu Woldie Yalew; Isabella Zouh; Christoph Gornott;handle: 10278/5060923
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Environmental Resear... arrow_drop_down Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2024License: CC BYData sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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more_vert Environmental Resear... arrow_drop_down Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2024License: CC BYData sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2024 Italy, GermanyPublisher:IOP Publishing Lisa Murken; Julia Tomalka; David Abigaba; Antwi-Bosiako Amoah; Joseph Armathé Amougou; Muriel Anaba; Ponraj Arumugam; Eres Awori; Hye-Rin Léa Baek; Till Below; Matti Cartsburg; Abel Chemura; Carla Cronauer; Iulii Didovets; Adefires Worku Gizaw; Stephanie Gleixner; Nele Gloy; Enrico Grams; Lemlem Habtemariam; Anna Hampf; Ylva Hauf; Tim Heckmann; Boubacar Ibrahim; Lennart Jansen; Francis Jarawura; Timothée Kagonbé; Juliane Kaufmann; Priscilla Kephe; Lena Klockemann; Stefan Lange; Rahel Laudien; Stefan Liersch; Naima Lipka; Sophia Lüttringhaus; Sibylla Neer; Oblé Neya; Steffen Noleppa; Sebastian Ostberg; Jonas Pollig; Paula Romanovska; Felicitas Röhrig; Bernhard Schauberger; Roopam Shukla; Lina Staubach; Mesmin Tchindjang; Sabine Undorf; Regina Vetter; Sophie von Loeben; Christoph von Stechow; Katarina von Witzke; Chiara Sophia Weituschat; Michel Wortmann; Amsalu Woldie Yalew; Isabella Zouh; Christoph Gornott;handle: 10278/5060923
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Environmental Resear... arrow_drop_down Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2024License: CC BYData sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type , Journal , Research 2013 Germany, France, United Kingdom, FrancePublisher:IOP Publishing Funded by:EC | ERMITAGEEC| ERMITAGEGerten, Dieter; Lucht, Wolfgang; Ostberg, Sebastian; Heinke, Jens; Kowarsch, Martin; Kreft, Holger; Kundzewicz, Zbigniew W.; Rastgooy, Johann; Warren, Rachel; Schellnhuber, Hans Joachim; Gerten, Dieter;; Lucht, Wolfgang;; Ostberg, Sebastian;; Heinke, Jens;; Kowarsch, Martin;; Kreft, Holger;; Kundzewicz, Zbigniew W;; Rastgooy, Johann;; Warren, Rachel;; Schellnhuber, Hans Joachim;;handle: 10568/34462
Cette étude de modélisation démontre à quel niveau d'élévation de la température moyenne mondiale (ΔTg) les régions seront exposées à des diminutions significatives de la disponibilité en eau douce et à des changements dans les écosystèmes terrestres. Les projections sont basées sur un nouvel ensemble cohérent de 152 scénarios climatiques (huit trajectoires ΔTg atteignant 1,5-5 ° C au-dessus des niveaux préindustriels d'ici 2100, chacune mise à l'échelle avec des schémas spatiaux de 19 modèles de circulation générale). Les résultats suggèrent que déjà à un ΔTg de 2 ° C et principalement dans les régions subtropicales, une pénurie d'eau plus élevée se produirait dans plus de 50% des 19 scénarios climatiques. D'importants changements biogéochimiques et structurels de la végétation se produiraient également à 2 ° C, mais principalement dans les écosystèmes subpolaires et semi-arides. D'autres régions seraient affectées à des niveaux de ΔTg plus élevés, avec une intensité plus faible ou avec une confiance plus faible. Au total, des niveaux moyens de réchauffement planétaire de 2 ° C, 3,5 ° C et 5 ° C sont simulés pour exposer 8%, 11% et 13% supplémentaires de la population mondiale à une pénurie d'eau nouvelle ou aggravée, respectivement, avec une confiance >50% (alors qu'environ1,3 milliard de personnes vivent déjà dans des régions pauvres en eau). Parallèlement, des transformations substantielles de l'habitat se produiraient dans les régions biogéographiques qui contiennent 1% (dans les zones touchées à 2 ° C), 10% (3,5 ° C) et 74% (5 ° C) des espèces de plantes vasculaires actuelles pondérées par l'endémisme, respectivement. Les résultats suggèrent une croissance non linéaire des impacts avec ΔTg et mettent en évidence les disparités régionales dans les amplitudes d'impact et les niveaux critiques de ΔTg. Este estudio de modelado demuestra a qué nivel de aumento de la temperatura media global (ΔTg) las regiones estarán expuestas a disminuciones significativas de la disponibilidad de agua dulce y cambios en los ecosistemas terrestres. Las proyecciones se basan en un nuevo conjunto consistente de 152 escenarios climáticos (ocho trayectorias de ΔTg que alcanzan 1.5–5 ° C por encima de los niveles preindustriales para 2100, cada una escalada con patrones espaciales de 19 modelos de circulación general). Los resultados sugieren que ya a una ΔTg de 2°C y principalmente en los subtrópicos, se produciría una mayor escasez de agua en >50% de los 19 escenarios climáticos. También se producirían cambios estructurales sustanciales biogeoquímicos y de vegetación a 2 ° C, pero principalmente en ecosistemas subpolares y semiáridos. Otras regiones se verían afectadas a niveles más altos de ΔTg, con menor intensidad o con menor confianza. En total, se simulan niveles medios de calentamiento global de 2 ° C, 3,5 ° C y 5 ° C para exponer a un 8%, 11% y 13% adicionales de la población mundial a una escasez de agua nueva o agravada, respectivamente, con >50% de confianza (mientras que ~1.300 millones de personas ya viven en regiones con escasez de agua). Al mismo tiempo, se producirían transformaciones sustanciales del hábitat en regiones biogeográficas que contienen el 1% (en zonas afectadas a 2 ° C), el 10% (3.5 ° C) y el 74% (5 ° C) de las especies de plantas vasculares ponderadas por endemismo actuales, respectivamente. Los resultados sugieren un crecimiento no lineal de los impactos junto con ΔTg y resaltan las disparidades regionales en las magnitudes de impacto y los niveles críticos de ΔTg. This modelling study demonstrates at what level of global mean temperature rise (ΔTg) regions will be exposed to significant decreases of freshwater availability and changes to terrestrial ecosystems. Projections are based on a new, consistent set of 152 climate scenarios (eight ΔTg trajectories reaching 1.5–5 ° C above pre-industrial levels by 2100, each scaled with spatial patterns from 19 general circulation models). The results suggest that already at a ΔTg of 2 ° C and mainly in the subtropics, higher water scarcity would occur in >50% out of the 19 climate scenarios. Substantial biogeochemical and vegetation structural changes would also occur at 2 ° C, but mainly in subpolar and semiarid ecosystems. Other regions would be affected at higher ΔTg levels, with lower intensity or with lower confidence. In total, mean global warming levels of 2 ° C, 3.5 ° C and 5 ° C are simulated to expose an additional 8%, 11% and 13% of the world population to new or aggravated water scarcity, respectively, with >50% confidence (while ∼1.3 billion people already live in water-scarce regions). Concurrently, substantial habitat transformations would occur in biogeographic regions that contain 1% (in zones affected at 2 ° C), 10% (3.5 ° C) and 74% (5 ° C) of present endemism-weighted vascular plant species, respectively. The results suggest nonlinear growth of impacts along with ΔTg and highlight regional disparities in impact magnitudes and critical ΔTg levels. توضح دراسة النمذجة هذه مستوى مناطق متوسط ارتفاع درجة الحرارة العالمية (ΔTg) التي ستتعرض لانخفاضات كبيرة في توافر المياه العذبة والتغيرات في النظم الإيكولوجية الأرضية. تستند التوقعات إلى مجموعة جديدة ومتسقة من 152 سيناريو مناخيًا (ثمانية مسارات ΔTg تصل إلى 1.5–5 درجة مئوية فوق مستويات ما قبل الصناعة بحلول عام 2100، تم قياس كل منها بأنماط مكانية من 19 نموذج دوران عام). تشير النتائج إلى أنه بالفعل عند درجة حرارة 2 درجة مئوية وبشكل أساسي في المناطق شبه الاستوائية، ستحدث ندرة مياه أعلى في أكثر من 50 ٪ من السيناريوهات المناخية التسعة عشر. كما ستحدث تغييرات هيكلية بيوكيميائية ونباتية كبيرة عند 2 درجة مئوية، ولكن بشكل أساسي في النظم الإيكولوجية تحت القطبية وشبه القاحلة. ستتأثر المناطق الأخرى عند مستويات ΔTg أعلى، بكثافة أقل أو بثقة أقل. في المجموع، تتم محاكاة متوسط مستويات الاحترار العالمي البالغة 2 درجة مئوية و 3.5 درجة مئوية و 5 درجات مئوية لتعريض 8 ٪ و 11 ٪ و 13 ٪ إضافية من سكان العالم لندرة المياه الجديدة أو المتفاقمة، على التوالي، بثقة >50 ٪ (في حين أن 1.3 مليار شخص يعيشون بالفعل في مناطق شحيحة المياه). وفي الوقت نفسه، ستحدث تحولات كبيرة في الموائل في المناطق الجغرافية الحيوية التي تحتوي على 1 ٪ (في المناطق المتأثرة عند 2 درجة مئوية) و 10 ٪ (3.5 درجة مئوية) و 74 ٪ (5 درجات مئوية) من أنواع النباتات الوعائية المتوطنة الحالية، على التوالي. تشير النتائج إلى نمو غير خطي للتأثيرات جنبًا إلى جنب مع ΔTg وتسلط الضوء على التفاوتات الإقليمية في أحجام التأثير ومستويات ΔTg الحرجة.
CGIAR CGSpace (Consu... arrow_drop_down CGIAR CGSpace (Consultative Group on International Agricultural Research)Article . 2014License: CC BYFull-Text: https://hdl.handle.net/10568/34462Data sources: Bielefeld Academic Search Engine (BASE)Publikationenserver der Georg-August-Universität GöttingenArticle . 2013 . Peer-reviewedLicense: CC BYGöttingen Research Online PublicationsArticle . 2017License: CC BYData sources: Göttingen Research Online PublicationsPublikationsserver der Humboldt-Universität zu BerlinArticle . 2013 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu BerlinUniversity of East Anglia: UEA Digital RepositoryArticle . 2013Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 58 citations 58 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!
visibility 83visibility views 83 download downloads 52 Powered bymore_vert CGIAR CGSpace (Consu... arrow_drop_down CGIAR CGSpace (Consultative Group on International Agricultural Research)Article . 2014License: CC BYFull-Text: https://hdl.handle.net/10568/34462Data sources: Bielefeld Academic Search Engine (BASE)Publikationenserver der Georg-August-Universität GöttingenArticle . 2013 . Peer-reviewedLicense: CC BYGöttingen Research Online PublicationsArticle . 2017License: CC BYData sources: Göttingen Research Online PublicationsPublikationsserver der Humboldt-Universität zu BerlinArticle . 2013 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu BerlinUniversity of East Anglia: UEA Digital RepositoryArticle . 2013Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type , Journal , Research 2013 Germany, France, United Kingdom, FrancePublisher:IOP Publishing Funded by:EC | ERMITAGEEC| ERMITAGEGerten, Dieter; Lucht, Wolfgang; Ostberg, Sebastian; Heinke, Jens; Kowarsch, Martin; Kreft, Holger; Kundzewicz, Zbigniew W.; Rastgooy, Johann; Warren, Rachel; Schellnhuber, Hans Joachim; Gerten, Dieter;; Lucht, Wolfgang;; Ostberg, Sebastian;; Heinke, Jens;; Kowarsch, Martin;; Kreft, Holger;; Kundzewicz, Zbigniew W;; Rastgooy, Johann;; Warren, Rachel;; Schellnhuber, Hans Joachim;;handle: 10568/34462
Cette étude de modélisation démontre à quel niveau d'élévation de la température moyenne mondiale (ΔTg) les régions seront exposées à des diminutions significatives de la disponibilité en eau douce et à des changements dans les écosystèmes terrestres. Les projections sont basées sur un nouvel ensemble cohérent de 152 scénarios climatiques (huit trajectoires ΔTg atteignant 1,5-5 ° C au-dessus des niveaux préindustriels d'ici 2100, chacune mise à l'échelle avec des schémas spatiaux de 19 modèles de circulation générale). Les résultats suggèrent que déjà à un ΔTg de 2 ° C et principalement dans les régions subtropicales, une pénurie d'eau plus élevée se produirait dans plus de 50% des 19 scénarios climatiques. D'importants changements biogéochimiques et structurels de la végétation se produiraient également à 2 ° C, mais principalement dans les écosystèmes subpolaires et semi-arides. D'autres régions seraient affectées à des niveaux de ΔTg plus élevés, avec une intensité plus faible ou avec une confiance plus faible. Au total, des niveaux moyens de réchauffement planétaire de 2 ° C, 3,5 ° C et 5 ° C sont simulés pour exposer 8%, 11% et 13% supplémentaires de la population mondiale à une pénurie d'eau nouvelle ou aggravée, respectivement, avec une confiance >50% (alors qu'environ1,3 milliard de personnes vivent déjà dans des régions pauvres en eau). Parallèlement, des transformations substantielles de l'habitat se produiraient dans les régions biogéographiques qui contiennent 1% (dans les zones touchées à 2 ° C), 10% (3,5 ° C) et 74% (5 ° C) des espèces de plantes vasculaires actuelles pondérées par l'endémisme, respectivement. Les résultats suggèrent une croissance non linéaire des impacts avec ΔTg et mettent en évidence les disparités régionales dans les amplitudes d'impact et les niveaux critiques de ΔTg. Este estudio de modelado demuestra a qué nivel de aumento de la temperatura media global (ΔTg) las regiones estarán expuestas a disminuciones significativas de la disponibilidad de agua dulce y cambios en los ecosistemas terrestres. Las proyecciones se basan en un nuevo conjunto consistente de 152 escenarios climáticos (ocho trayectorias de ΔTg que alcanzan 1.5–5 ° C por encima de los niveles preindustriales para 2100, cada una escalada con patrones espaciales de 19 modelos de circulación general). Los resultados sugieren que ya a una ΔTg de 2°C y principalmente en los subtrópicos, se produciría una mayor escasez de agua en >50% de los 19 escenarios climáticos. También se producirían cambios estructurales sustanciales biogeoquímicos y de vegetación a 2 ° C, pero principalmente en ecosistemas subpolares y semiáridos. Otras regiones se verían afectadas a niveles más altos de ΔTg, con menor intensidad o con menor confianza. En total, se simulan niveles medios de calentamiento global de 2 ° C, 3,5 ° C y 5 ° C para exponer a un 8%, 11% y 13% adicionales de la población mundial a una escasez de agua nueva o agravada, respectivamente, con >50% de confianza (mientras que ~1.300 millones de personas ya viven en regiones con escasez de agua). Al mismo tiempo, se producirían transformaciones sustanciales del hábitat en regiones biogeográficas que contienen el 1% (en zonas afectadas a 2 ° C), el 10% (3.5 ° C) y el 74% (5 ° C) de las especies de plantas vasculares ponderadas por endemismo actuales, respectivamente. Los resultados sugieren un crecimiento no lineal de los impactos junto con ΔTg y resaltan las disparidades regionales en las magnitudes de impacto y los niveles críticos de ΔTg. This modelling study demonstrates at what level of global mean temperature rise (ΔTg) regions will be exposed to significant decreases of freshwater availability and changes to terrestrial ecosystems. Projections are based on a new, consistent set of 152 climate scenarios (eight ΔTg trajectories reaching 1.5–5 ° C above pre-industrial levels by 2100, each scaled with spatial patterns from 19 general circulation models). The results suggest that already at a ΔTg of 2 ° C and mainly in the subtropics, higher water scarcity would occur in >50% out of the 19 climate scenarios. Substantial biogeochemical and vegetation structural changes would also occur at 2 ° C, but mainly in subpolar and semiarid ecosystems. Other regions would be affected at higher ΔTg levels, with lower intensity or with lower confidence. In total, mean global warming levels of 2 ° C, 3.5 ° C and 5 ° C are simulated to expose an additional 8%, 11% and 13% of the world population to new or aggravated water scarcity, respectively, with >50% confidence (while ∼1.3 billion people already live in water-scarce regions). Concurrently, substantial habitat transformations would occur in biogeographic regions that contain 1% (in zones affected at 2 ° C), 10% (3.5 ° C) and 74% (5 ° C) of present endemism-weighted vascular plant species, respectively. The results suggest nonlinear growth of impacts along with ΔTg and highlight regional disparities in impact magnitudes and critical ΔTg levels. توضح دراسة النمذجة هذه مستوى مناطق متوسط ارتفاع درجة الحرارة العالمية (ΔTg) التي ستتعرض لانخفاضات كبيرة في توافر المياه العذبة والتغيرات في النظم الإيكولوجية الأرضية. تستند التوقعات إلى مجموعة جديدة ومتسقة من 152 سيناريو مناخيًا (ثمانية مسارات ΔTg تصل إلى 1.5–5 درجة مئوية فوق مستويات ما قبل الصناعة بحلول عام 2100، تم قياس كل منها بأنماط مكانية من 19 نموذج دوران عام). تشير النتائج إلى أنه بالفعل عند درجة حرارة 2 درجة مئوية وبشكل أساسي في المناطق شبه الاستوائية، ستحدث ندرة مياه أعلى في أكثر من 50 ٪ من السيناريوهات المناخية التسعة عشر. كما ستحدث تغييرات هيكلية بيوكيميائية ونباتية كبيرة عند 2 درجة مئوية، ولكن بشكل أساسي في النظم الإيكولوجية تحت القطبية وشبه القاحلة. ستتأثر المناطق الأخرى عند مستويات ΔTg أعلى، بكثافة أقل أو بثقة أقل. في المجموع، تتم محاكاة متوسط مستويات الاحترار العالمي البالغة 2 درجة مئوية و 3.5 درجة مئوية و 5 درجات مئوية لتعريض 8 ٪ و 11 ٪ و 13 ٪ إضافية من سكان العالم لندرة المياه الجديدة أو المتفاقمة، على التوالي، بثقة >50 ٪ (في حين أن 1.3 مليار شخص يعيشون بالفعل في مناطق شحيحة المياه). وفي الوقت نفسه، ستحدث تحولات كبيرة في الموائل في المناطق الجغرافية الحيوية التي تحتوي على 1 ٪ (في المناطق المتأثرة عند 2 درجة مئوية) و 10 ٪ (3.5 درجة مئوية) و 74 ٪ (5 درجات مئوية) من أنواع النباتات الوعائية المتوطنة الحالية، على التوالي. تشير النتائج إلى نمو غير خطي للتأثيرات جنبًا إلى جنب مع ΔTg وتسلط الضوء على التفاوتات الإقليمية في أحجام التأثير ومستويات ΔTg الحرجة.
CGIAR CGSpace (Consu... arrow_drop_down CGIAR CGSpace (Consultative Group on International Agricultural Research)Article . 2014License: CC BYFull-Text: https://hdl.handle.net/10568/34462Data sources: Bielefeld Academic Search Engine (BASE)Publikationenserver der Georg-August-Universität GöttingenArticle . 2013 . Peer-reviewedLicense: CC BYGöttingen Research Online PublicationsArticle . 2017License: CC BYData sources: Göttingen Research Online PublicationsPublikationsserver der Humboldt-Universität zu BerlinArticle . 2013 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu BerlinUniversity of East Anglia: UEA Digital RepositoryArticle . 2013Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 58 citations 58 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!
visibility 83visibility views 83 download downloads 52 Powered bymore_vert CGIAR CGSpace (Consu... arrow_drop_down CGIAR CGSpace (Consultative Group on International Agricultural Research)Article . 2014License: CC BYFull-Text: https://hdl.handle.net/10568/34462Data sources: Bielefeld Academic Search Engine (BASE)Publikationenserver der Georg-August-Universität GöttingenArticle . 2013 . Peer-reviewedLicense: CC BYGöttingen Research Online PublicationsArticle . 2017License: CC BYData sources: Göttingen Research Online PublicationsPublikationsserver der Humboldt-Universität zu BerlinArticle . 2013 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu BerlinUniversity of East Anglia: UEA Digital RepositoryArticle . 2013Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type 2012Publisher:Copernicus GmbH Jens Heinke; Sebastian Ostberg; Sibyll Schaphoff; Katja Frieler; Christoph Müller; Dieter Gerten; Malte Meinshausen; Wolfgang Lucht;Abstract. In the ongoing political debate on climate change, global mean temperature change (ΔTglob) has become the yardstick by which mitigation costs, impacts from unavoided climate change, and adaptation requirements are discussed. For a scientifically informed discourse along these lines systematic assessments of climate change impacts as a function of ΔTglob are required. The current availability of climate change scenarios constrains this type of assessment to a narrow range of temperature change and/or a reduced ensemble of climate models. Here, a newly composed dataset of climate change scenarios is presented that addresses the specific requirements for global assessments of climate change impacts as a function of ΔTglob. A pattern-scaling approach is applied to extract generalized patterns of spatially explicit change in temperature, precipitation and cloudiness from 19 AOGCMs. The patterns are combined with scenarios of global mean temperature increase obtained from the reduced-complexity climate model MAGICC6 to create climate scenarios covering warming levels from 1.5 to 5 degrees above pre-industrial levels around the year 2100. The patterns are shown to sufficiently maintain the original AOGCMs' climate change properties, even though they, necessarily, utilize a simplified relationships between ΔTglob and changes in local climate properties. The dataset (made available online upon final publication of this paper) facilitates systematic analyses of climate change impacts as it covers a wider and finer-spaced range of climate change scenarios than the original AOGCM simulations.
https://doi.org/10.5... arrow_drop_down https://doi.org/10.5194/gmdd-5...Article . 2012 . Peer-reviewedLicense: CC BYData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess Routeshybrid 8 citations 8 popularity Average influence Top 10% impulse Top 10% Powered by BIP!
more_vert https://doi.org/10.5... arrow_drop_down https://doi.org/10.5194/gmdd-5...Article . 2012 . Peer-reviewedLicense: CC BYData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type 2012Publisher:Copernicus GmbH Jens Heinke; Sebastian Ostberg; Sibyll Schaphoff; Katja Frieler; Christoph Müller; Dieter Gerten; Malte Meinshausen; Wolfgang Lucht;Abstract. In the ongoing political debate on climate change, global mean temperature change (ΔTglob) has become the yardstick by which mitigation costs, impacts from unavoided climate change, and adaptation requirements are discussed. For a scientifically informed discourse along these lines systematic assessments of climate change impacts as a function of ΔTglob are required. The current availability of climate change scenarios constrains this type of assessment to a narrow range of temperature change and/or a reduced ensemble of climate models. Here, a newly composed dataset of climate change scenarios is presented that addresses the specific requirements for global assessments of climate change impacts as a function of ΔTglob. A pattern-scaling approach is applied to extract generalized patterns of spatially explicit change in temperature, precipitation and cloudiness from 19 AOGCMs. The patterns are combined with scenarios of global mean temperature increase obtained from the reduced-complexity climate model MAGICC6 to create climate scenarios covering warming levels from 1.5 to 5 degrees above pre-industrial levels around the year 2100. The patterns are shown to sufficiently maintain the original AOGCMs' climate change properties, even though they, necessarily, utilize a simplified relationships between ΔTglob and changes in local climate properties. The dataset (made available online upon final publication of this paper) facilitates systematic analyses of climate change impacts as it covers a wider and finer-spaced range of climate change scenarios than the original AOGCM simulations.
https://doi.org/10.5... arrow_drop_down https://doi.org/10.5194/gmdd-5...Article . 2012 . Peer-reviewedLicense: CC BYData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess Routeshybrid 8 citations 8 popularity Average influence Top 10% impulse Top 10% Powered by BIP!
more_vert https://doi.org/10.5... arrow_drop_down https://doi.org/10.5194/gmdd-5...Article . 2012 . Peer-reviewedLicense: CC BYData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Conference object , Journal 2018 Germany, France, France, France, FrancePublisher:IOP Publishing Funded by:NSF | Collaborative Research: E..., NSF | CNH: Pluvials, Droughts, ..., EC | HELIXNSF| Collaborative Research: EaSM2--Wildfires and Regional Climate Variability - Mechanisms, Modeling, and Prediction ,NSF| CNH: Pluvials, Droughts, Energetics, and the Mongol Empire ,EC| HELIXJia Yang; Kazuya Nishina; Richard Betts; Richard Betts; Sibyll Schaphoff; Louis François; Alexandra-Jane Henrot; Jinfeng Chang; Christopher P. O. Reyer; Catherine Morfopoulos; Katja Frieler; Philippe Ciais; Jörg Steinkamp; Rashid Rafique; Fang Zhao; Thomas Hickler; Hanqin Tian; Sebastian Ostberg; Anselmo García Cantú; Akihiko Ito; Shufen Pan;This paper evaluates the ability of eight global vegetation models to reproduce recent trends and inter-annual variability of biomass in natural terrestrial ecosystems. For the purpose of this evaluation, the simulated trajectories of biomass are expressed in terms of the relative rate of change in biomass (RRB), defined as the deviation of the actual rate of biomass turnover from its equilibrium counterpart. Cumulative changes in RRB explain long-term changes in biomass pools. RRB simulated by the global vegetation models is compared with its observational equivalent, derived from vegetation optical depth reconstructions of above-ground biomass (AGB) over the period 1993–2010. According to the RRB analysis, the rate of global biomass growth described by the ensemble of simulations substantially exceeds the observation. The observed fluctuations of global RRB are significantly correlated with El Niño Southern Oscillation events (ENSO), but only some of the simulations reproduce this correlation. However, the ENSO sensitivity of RRB in the tropics is not significant in the observation, while it is in some of the simulations. This mismatch points to an important limitation of the observed AGB reconstruction to capture biomass variations in tropical forests. Important discrepancies in RRB were also identified at the regional scale, in the tropical forests of Amazonia and Central Africa, as well as in the boreal forests of north-western America, western and central Siberia. In each of these regions, the RRBs derived from the simulations were analyzed in connection with underlying differences in net primary productivity and biomass turnover rate ̶as a basis for exploring in how far differences in simulated changes in biomass are attributed to the response of the carbon uptake to CO _2 increments, as well as to the model representation of factors affecting the rates of mortality and turnover of foliage and roots. Overall, our findings stress the usefulness of using RRB to evaluate complex vegetation models and highlight the importance of conducting further evaluations of both the actual rate of biomass turnover and its equilibrium counterpart, with special focus on their background values and sources of variation. In turn, this task would require the availability of more accurate multi-year observational data of biomass and net primary productivity for natural ecosystems, as well as detailed and updated information on land-cover classification.
Hyper Article en Lig... arrow_drop_down Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2018Full-Text: https://hal.science/hal-02903437Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2018Full-Text: https://hal.science/hal-02903437Data sources: Bielefeld Academic Search Engine (BASE)Fachrepositorium LebenswissenschaftenArticle . 2018License: CC BYData sources: Fachrepositorium Lebenswissenschaftenadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 3 citations 3 popularity Average influence Average impulse Average Powered by BIP!
more_vert Hyper Article en Lig... arrow_drop_down Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2018Full-Text: https://hal.science/hal-02903437Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2018Full-Text: https://hal.science/hal-02903437Data sources: Bielefeld Academic Search Engine (BASE)Fachrepositorium LebenswissenschaftenArticle . 2018License: CC BYData sources: Fachrepositorium Lebenswissenschaftenadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1088/1748-9326/aac63c&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Conference object , Journal 2018 Germany, France, France, France, FrancePublisher:IOP Publishing Funded by:NSF | Collaborative Research: E..., NSF | CNH: Pluvials, Droughts, ..., EC | HELIXNSF| Collaborative Research: EaSM2--Wildfires and Regional Climate Variability - Mechanisms, Modeling, and Prediction ,NSF| CNH: Pluvials, Droughts, Energetics, and the Mongol Empire ,EC| HELIXJia Yang; Kazuya Nishina; Richard Betts; Richard Betts; Sibyll Schaphoff; Louis François; Alexandra-Jane Henrot; Jinfeng Chang; Christopher P. O. Reyer; Catherine Morfopoulos; Katja Frieler; Philippe Ciais; Jörg Steinkamp; Rashid Rafique; Fang Zhao; Thomas Hickler; Hanqin Tian; Sebastian Ostberg; Anselmo García Cantú; Akihiko Ito; Shufen Pan;This paper evaluates the ability of eight global vegetation models to reproduce recent trends and inter-annual variability of biomass in natural terrestrial ecosystems. For the purpose of this evaluation, the simulated trajectories of biomass are expressed in terms of the relative rate of change in biomass (RRB), defined as the deviation of the actual rate of biomass turnover from its equilibrium counterpart. Cumulative changes in RRB explain long-term changes in biomass pools. RRB simulated by the global vegetation models is compared with its observational equivalent, derived from vegetation optical depth reconstructions of above-ground biomass (AGB) over the period 1993–2010. According to the RRB analysis, the rate of global biomass growth described by the ensemble of simulations substantially exceeds the observation. The observed fluctuations of global RRB are significantly correlated with El Niño Southern Oscillation events (ENSO), but only some of the simulations reproduce this correlation. However, the ENSO sensitivity of RRB in the tropics is not significant in the observation, while it is in some of the simulations. This mismatch points to an important limitation of the observed AGB reconstruction to capture biomass variations in tropical forests. Important discrepancies in RRB were also identified at the regional scale, in the tropical forests of Amazonia and Central Africa, as well as in the boreal forests of north-western America, western and central Siberia. In each of these regions, the RRBs derived from the simulations were analyzed in connection with underlying differences in net primary productivity and biomass turnover rate ̶as a basis for exploring in how far differences in simulated changes in biomass are attributed to the response of the carbon uptake to CO _2 increments, as well as to the model representation of factors affecting the rates of mortality and turnover of foliage and roots. Overall, our findings stress the usefulness of using RRB to evaluate complex vegetation models and highlight the importance of conducting further evaluations of both the actual rate of biomass turnover and its equilibrium counterpart, with special focus on their background values and sources of variation. In turn, this task would require the availability of more accurate multi-year observational data of biomass and net primary productivity for natural ecosystems, as well as detailed and updated information on land-cover classification.
Hyper Article en Lig... arrow_drop_down Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2018Full-Text: https://hal.science/hal-02903437Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2018Full-Text: https://hal.science/hal-02903437Data sources: Bielefeld Academic Search Engine (BASE)Fachrepositorium LebenswissenschaftenArticle . 2018License: CC BYData sources: Fachrepositorium Lebenswissenschaftenadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 3 citations 3 popularity Average influence Average impulse Average Powered by BIP!
more_vert Hyper Article en Lig... arrow_drop_down Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2018Full-Text: https://hal.science/hal-02903437Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2018Full-Text: https://hal.science/hal-02903437Data sources: Bielefeld Academic Search Engine (BASE)Fachrepositorium LebenswissenschaftenArticle . 2018License: CC BYData sources: Fachrepositorium Lebenswissenschaftenadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Conference object , Other literature type , Journal 2019Embargo end date: 16 Mar 2019 Netherlands, France, United Kingdom, Germany, Switzerland, France, France, France, France, Japan, France, Netherlands, Netherlands, Canada, Spain, France, AustriaPublisher:Springer Science and Business Media LLC Funded by:EC | IMPACT2C, EC | HELIXEC| IMPACT2C ,EC| HELIXJeroen Steenbeek; Erwin Schmid; Tyler D. Eddy; Tyler D. Eddy; Tyler D. Eddy; Derek P. Tittensor; Derek P. Tittensor; Rene Orth; Rene Orth; Yadu Pokhrel; Joshua Elliott; Yusuke Satoh; Yusuke Satoh; Christian Folberth; Louis François; Andrew D. Friend; Catherine Morfopoulos; Nikolay Khabarov; Peter Lawrence; Naota Hanasaki; Michelle T. H. van Vliet; Akihiko Ito; Sonia I. Seneviratne; Veronika Huber; Thomas A. M. Pugh; Jinfeng Chang; Tobias Stacke; Philippe Ciais; Lila Warszawski; Jan Volkholz; Matthias Büchner; Yoshihide Wada; Christopher P. O. Reyer; Xuhui Wang; Xuhui Wang; Xuhui Wang; Dieter Gerten; Dieter Gerten; Sebastian Ostberg; Qiuhong Tang; Gen Sakurai; David A. Carozza; David A. Carozza; Christoph Müller; Jacob Schewe; Lutz Breuer; Delphine Deryng; Heike K. Lotze; Hannes Müller Schmied; Robert Vautard; Hyungjun Kim; Fang Zhao; Allard de Wit; Jörg Steinkamp; Katja Frieler; Simon N. Gosling; Lukas Gudmundsson; Marta Coll; Hanqin Tian;doi: 10.1038/s41467-019-08745-6 , 10.17863/cam.37807 , 10.60692/8dj48-81382 , 10.3929/ethz-b-000330244 , 10.60692/8mcvk-e7225
pmid: 30824763
pmc: PMC6397256
handle: 10261/181642
doi: 10.1038/s41467-019-08745-6 , 10.17863/cam.37807 , 10.60692/8dj48-81382 , 10.3929/ethz-b-000330244 , 10.60692/8mcvk-e7225
pmid: 30824763
pmc: PMC6397256
handle: 10261/181642
AbstractGlobal impact models represent process-level understanding of how natural and human systems may be affected by climate change. Their projections are used in integrated assessments of climate change. Here we test, for the first time, systematically across many important systems, how well such impact models capture the impacts of extreme climate conditions. Using the 2003 European heat wave and drought as a historical analogue for comparable events in the future, we find that a majority of models underestimate the extremeness of impacts in important sectors such as agriculture, terrestrial ecosystems, and heat-related human mortality, while impacts on water resources and hydropower are overestimated in some river basins; and the spread across models is often large. This has important implications for economic assessments of climate change impacts that rely on these models. It also means that societal risks from future extreme events may be greater than previously thought.
IIASA PURE arrow_drop_down Université Jean Monnet – Saint-Etienne: HALArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)École Polytechnique, Université Paris-Saclay: HALArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Memorial University of Newfoundland: Research RepositoryArticle . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Recolector de Ciencia Abierta, RECOLECTAArticle . 2019 . Peer-reviewedData sources: Recolector de Ciencia Abierta, RECOLECTAWageningen Staff PublicationsArticle . 2019License: CC BYData sources: Wageningen Staff PublicationsHochschulschriftenserver - Universität Frankfurt am MainArticle . 2019Data sources: Hochschulschriftenserver - Universität Frankfurt am MainPublication Server of Goethe University Frankfurt am MainArticle . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen 202 citations 202 popularity Top 0.1% influence Top 10% impulse Top 0.1% Powered by BIP!
more_vert IIASA PURE arrow_drop_down Université Jean Monnet – Saint-Etienne: HALArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)École Polytechnique, Université Paris-Saclay: HALArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Memorial University of Newfoundland: Research RepositoryArticle . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Recolector de Ciencia Abierta, RECOLECTAArticle . 2019 . Peer-reviewedData sources: Recolector de Ciencia Abierta, RECOLECTAWageningen Staff PublicationsArticle . 2019License: CC BYData sources: Wageningen Staff PublicationsHochschulschriftenserver - Universität Frankfurt am MainArticle . 2019Data sources: Hochschulschriftenserver - Universität Frankfurt am MainPublication Server of Goethe University Frankfurt am MainArticle . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1038/s41467-019-08745-6&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Conference object , Other literature type , Journal 2019Embargo end date: 16 Mar 2019 Netherlands, France, United Kingdom, Germany, Switzerland, France, France, France, France, Japan, France, Netherlands, Netherlands, Canada, Spain, France, AustriaPublisher:Springer Science and Business Media LLC Funded by:EC | IMPACT2C, EC | HELIXEC| IMPACT2C ,EC| HELIXJeroen Steenbeek; Erwin Schmid; Tyler D. Eddy; Tyler D. Eddy; Tyler D. Eddy; Derek P. Tittensor; Derek P. Tittensor; Rene Orth; Rene Orth; Yadu Pokhrel; Joshua Elliott; Yusuke Satoh; Yusuke Satoh; Christian Folberth; Louis François; Andrew D. Friend; Catherine Morfopoulos; Nikolay Khabarov; Peter Lawrence; Naota Hanasaki; Michelle T. H. van Vliet; Akihiko Ito; Sonia I. Seneviratne; Veronika Huber; Thomas A. M. Pugh; Jinfeng Chang; Tobias Stacke; Philippe Ciais; Lila Warszawski; Jan Volkholz; Matthias Büchner; Yoshihide Wada; Christopher P. O. Reyer; Xuhui Wang; Xuhui Wang; Xuhui Wang; Dieter Gerten; Dieter Gerten; Sebastian Ostberg; Qiuhong Tang; Gen Sakurai; David A. Carozza; David A. Carozza; Christoph Müller; Jacob Schewe; Lutz Breuer; Delphine Deryng; Heike K. Lotze; Hannes Müller Schmied; Robert Vautard; Hyungjun Kim; Fang Zhao; Allard de Wit; Jörg Steinkamp; Katja Frieler; Simon N. Gosling; Lukas Gudmundsson; Marta Coll; Hanqin Tian;doi: 10.1038/s41467-019-08745-6 , 10.17863/cam.37807 , 10.60692/8dj48-81382 , 10.3929/ethz-b-000330244 , 10.60692/8mcvk-e7225
pmid: 30824763
pmc: PMC6397256
handle: 10261/181642
doi: 10.1038/s41467-019-08745-6 , 10.17863/cam.37807 , 10.60692/8dj48-81382 , 10.3929/ethz-b-000330244 , 10.60692/8mcvk-e7225
pmid: 30824763
pmc: PMC6397256
handle: 10261/181642
AbstractGlobal impact models represent process-level understanding of how natural and human systems may be affected by climate change. Their projections are used in integrated assessments of climate change. Here we test, for the first time, systematically across many important systems, how well such impact models capture the impacts of extreme climate conditions. Using the 2003 European heat wave and drought as a historical analogue for comparable events in the future, we find that a majority of models underestimate the extremeness of impacts in important sectors such as agriculture, terrestrial ecosystems, and heat-related human mortality, while impacts on water resources and hydropower are overestimated in some river basins; and the spread across models is often large. This has important implications for economic assessments of climate change impacts that rely on these models. It also means that societal risks from future extreme events may be greater than previously thought.
IIASA PURE arrow_drop_down Université Jean Monnet – Saint-Etienne: HALArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)École Polytechnique, Université Paris-Saclay: HALArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Memorial University of Newfoundland: Research RepositoryArticle . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Recolector de Ciencia Abierta, RECOLECTAArticle . 2019 . Peer-reviewedData sources: Recolector de Ciencia Abierta, RECOLECTAWageningen Staff PublicationsArticle . 2019License: CC BYData sources: Wageningen Staff PublicationsHochschulschriftenserver - Universität Frankfurt am MainArticle . 2019Data sources: Hochschulschriftenserver - Universität Frankfurt am MainPublication Server of Goethe University Frankfurt am MainArticle . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1038/s41467-019-08745-6&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen 202 citations 202 popularity Top 0.1% influence Top 10% impulse Top 0.1% Powered by BIP!
more_vert IIASA PURE arrow_drop_down Université Jean Monnet – Saint-Etienne: HALArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)École Polytechnique, Université Paris-Saclay: HALArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Memorial University of Newfoundland: Research RepositoryArticle . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Recolector de Ciencia Abierta, RECOLECTAArticle . 2019 . Peer-reviewedData sources: Recolector de Ciencia Abierta, RECOLECTAWageningen Staff PublicationsArticle . 2019License: CC BYData sources: Wageningen Staff PublicationsHochschulschriftenserver - Universität Frankfurt am MainArticle . 2019Data sources: Hochschulschriftenserver - Universität Frankfurt am MainPublication Server of Goethe University Frankfurt am MainArticle . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1038/s41467-019-08745-6&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Journal 2013 Germany, France, United Kingdom, France, France, France, France, United KingdomPublisher:Proceedings of the National Academy of Sciences Funded by:EC | GREENCYCLESIIEC| GREENCYCLESIIAndrew D. Friend; F. Ian Woodward; Tim T. Rademacher; Ron Kahana; Sibyll Schaphoff; Richard Betts; Akihiko Ito; Andy Wiltshire; Rutger Dankers; Axel Kleidon; Pete Falloon; Wolfgang Lucht; Wolfgang Lucht; Philippe Ciais; Lila Warszawski; Nicolas Vuichard; Philippe Peylin; Patricia Cadule; Mark R. Lomas; Rozenn Keribin; Douglas B. Clark; Sebastian Ostberg; Kazuya Nishina; Ryan Pavlick;Future climate change and increasing atmospheric CO 2 are expected to cause major changes in vegetation structure and function over large fractions of the global land surface. Seven global vegetation models are used to analyze possible responses to future climate simulated by a range of general circulation models run under all four representative concentration pathway scenarios of changing concentrations of greenhouse gases. All 110 simulations predict an increase in global vegetation carbon to 2100, but with substantial variation between vegetation models. For example, at 4 °C of global land surface warming (510–758 ppm of CO 2 ), vegetation carbon increases by 52–477 Pg C (224 Pg C mean), mainly due to CO 2 fertilization of photosynthesis. Simulations agree on large regional increases across much of the boreal forest, western Amazonia, central Africa, western China, and southeast Asia, with reductions across southwestern North America, central South America, southern Mediterranean areas, southwestern Africa, and southwestern Australia. Four vegetation models display discontinuities across 4 °C of warming, indicating global thresholds in the balance of positive and negative influences on productivity and biomass. In contrast to previous global vegetation model studies, we emphasize the importance of uncertainties in projected changes in carbon residence times. We find, when all seven models are considered for one representative concentration pathway × general circulation model combination, such uncertainties explain 30% more variation in modeled vegetation carbon change than responses of net primary productivity alone, increasing to 151% for non-HYBRID4 models. A change in research priorities away from production and toward structural dynamics and demographic processes is recommended.
Proceedings of the N... arrow_drop_down Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2014Data sources: Bielefeld Academic Search Engine (BASE)Proceedings of the National Academy of SciencesArticle . 2013 . Peer-reviewedData sources: CrossrefÉcole Polytechnique, Université Paris-Saclay: HALArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Natural Environment Research Council: NERC Open Research ArchiveArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1073/pnas.1222477110&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen bronze 465 citations 465 popularity Top 0.1% influence Top 1% impulse Top 0.1% Powered by BIP!
more_vert Proceedings of the N... arrow_drop_down Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2014Data sources: Bielefeld Academic Search Engine (BASE)Proceedings of the National Academy of SciencesArticle . 2013 . Peer-reviewedData sources: CrossrefÉcole Polytechnique, Université Paris-Saclay: HALArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Natural Environment Research Council: NERC Open Research ArchiveArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1073/pnas.1222477110&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Journal 2013 Germany, France, United Kingdom, France, France, France, France, United KingdomPublisher:Proceedings of the National Academy of Sciences Funded by:EC | GREENCYCLESIIEC| GREENCYCLESIIAndrew D. Friend; F. Ian Woodward; Tim T. Rademacher; Ron Kahana; Sibyll Schaphoff; Richard Betts; Akihiko Ito; Andy Wiltshire; Rutger Dankers; Axel Kleidon; Pete Falloon; Wolfgang Lucht; Wolfgang Lucht; Philippe Ciais; Lila Warszawski; Nicolas Vuichard; Philippe Peylin; Patricia Cadule; Mark R. Lomas; Rozenn Keribin; Douglas B. Clark; Sebastian Ostberg; Kazuya Nishina; Ryan Pavlick;Future climate change and increasing atmospheric CO 2 are expected to cause major changes in vegetation structure and function over large fractions of the global land surface. Seven global vegetation models are used to analyze possible responses to future climate simulated by a range of general circulation models run under all four representative concentration pathway scenarios of changing concentrations of greenhouse gases. All 110 simulations predict an increase in global vegetation carbon to 2100, but with substantial variation between vegetation models. For example, at 4 °C of global land surface warming (510–758 ppm of CO 2 ), vegetation carbon increases by 52–477 Pg C (224 Pg C mean), mainly due to CO 2 fertilization of photosynthesis. Simulations agree on large regional increases across much of the boreal forest, western Amazonia, central Africa, western China, and southeast Asia, with reductions across southwestern North America, central South America, southern Mediterranean areas, southwestern Africa, and southwestern Australia. Four vegetation models display discontinuities across 4 °C of warming, indicating global thresholds in the balance of positive and negative influences on productivity and biomass. In contrast to previous global vegetation model studies, we emphasize the importance of uncertainties in projected changes in carbon residence times. We find, when all seven models are considered for one representative concentration pathway × general circulation model combination, such uncertainties explain 30% more variation in modeled vegetation carbon change than responses of net primary productivity alone, increasing to 151% for non-HYBRID4 models. A change in research priorities away from production and toward structural dynamics and demographic processes is recommended.
Proceedings of the N... arrow_drop_down Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2014Data sources: Bielefeld Academic Search Engine (BASE)Proceedings of the National Academy of SciencesArticle . 2013 . Peer-reviewedData sources: CrossrefÉcole Polytechnique, Université Paris-Saclay: HALArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Natural Environment Research Council: NERC Open Research ArchiveArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1073/pnas.1222477110&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen bronze 465 citations 465 popularity Top 0.1% influence Top 1% impulse Top 0.1% Powered by BIP!
more_vert Proceedings of the N... arrow_drop_down Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2014Data sources: Bielefeld Academic Search Engine (BASE)Proceedings of the National Academy of SciencesArticle . 2013 . Peer-reviewedData sources: CrossrefÉcole Polytechnique, Université Paris-Saclay: HALArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Natural Environment Research Council: NERC Open Research ArchiveArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1073/pnas.1222477110&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Journal 2018Embargo end date: 01 Sep 2022 GermanyPublisher:IOP Publishing Sebastian Ostberg; Sebastian Ostberg; Petra Döll; Dieter Gerten; Dieter Gerten; Hannes Müller Schmied; Tim Trautmann; Fahad Saaed; Carl-Friedrich Schleussner; Carl-Friedrich Schleussner;To support implementation of the Paris Agreement, the new HAPPI ensemble of 20 bias-corrected simulations of four climate models was used to drive two global hydrological models, WaterGAP and LPJmL, for assessing freshwater-related hazards and risks in worlds approximately 1.5 °C and 2 °C warmer than pre-industrial. Quasi-stationary HAPPI simulations are better suited than transient CMIP-like simulations for assessing hazards at the two targeted long-term global warming (GW) levels. We analyzed seven hydrological hazard indicators that characterize freshwater-related hazards for humans, freshwater biota and vegetation. Using a strict definition for significant differences, we identified for all but one indicator that areas with either significantly wetter or drier conditions (calculated as percent changes from 2006–2015) are smaller in the 1.5 °C world. For example, 7 day high flow is projected to increase significantly on 11% and 21% of the global land area at 1.5 °C and 2 °C, respectively. However, differences between hydrological hazards at the two GW levels are significant on less than 12% of the area. GW affects a larger area and more people by increases—rather than by decreases—of mean annual and 1-in-10 dry year streamflow, 7 day high flow, and groundwater recharge. The opposite is true for 7 day low flow, maximum snow storage, and soil moisture in the driest month of the growing period. Mean annual streamflow shows the lowest projected percent changes of all indicators. Among country groups, low income countries and lower middle income countries are most affected by decreased low flows and increased high flows, respectively, while high income countries are least affected by such changes. The incremental impact between 1.5 °C and 2 °C on high flows would be felt most by low income and lower middle income countries, the effect on soil moisture and low flows most by high income countries.
Publication Database... arrow_drop_down Fachrepositorium LebenswissenschaftenArticle . 2018License: CC BYData sources: Fachrepositorium LebenswissenschaftenPublikationsserver der Humboldt-Universität zu BerlinArticle . 2018 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu Berlinadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1088/1748-9326/aab792&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 77 citations 77 popularity Top 1% influence Top 10% impulse Top 1% Powered by BIP!
visibility 64visibility views 64 download downloads 31 Powered bymore_vert Publication Database... arrow_drop_down Fachrepositorium LebenswissenschaftenArticle . 2018License: CC BYData sources: Fachrepositorium LebenswissenschaftenPublikationsserver der Humboldt-Universität zu BerlinArticle . 2018 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu Berlinadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1088/1748-9326/aab792&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Journal 2018Embargo end date: 01 Sep 2022 GermanyPublisher:IOP Publishing Sebastian Ostberg; Sebastian Ostberg; Petra Döll; Dieter Gerten; Dieter Gerten; Hannes Müller Schmied; Tim Trautmann; Fahad Saaed; Carl-Friedrich Schleussner; Carl-Friedrich Schleussner;To support implementation of the Paris Agreement, the new HAPPI ensemble of 20 bias-corrected simulations of four climate models was used to drive two global hydrological models, WaterGAP and LPJmL, for assessing freshwater-related hazards and risks in worlds approximately 1.5 °C and 2 °C warmer than pre-industrial. Quasi-stationary HAPPI simulations are better suited than transient CMIP-like simulations for assessing hazards at the two targeted long-term global warming (GW) levels. We analyzed seven hydrological hazard indicators that characterize freshwater-related hazards for humans, freshwater biota and vegetation. Using a strict definition for significant differences, we identified for all but one indicator that areas with either significantly wetter or drier conditions (calculated as percent changes from 2006–2015) are smaller in the 1.5 °C world. For example, 7 day high flow is projected to increase significantly on 11% and 21% of the global land area at 1.5 °C and 2 °C, respectively. However, differences between hydrological hazards at the two GW levels are significant on less than 12% of the area. GW affects a larger area and more people by increases—rather than by decreases—of mean annual and 1-in-10 dry year streamflow, 7 day high flow, and groundwater recharge. The opposite is true for 7 day low flow, maximum snow storage, and soil moisture in the driest month of the growing period. Mean annual streamflow shows the lowest projected percent changes of all indicators. Among country groups, low income countries and lower middle income countries are most affected by decreased low flows and increased high flows, respectively, while high income countries are least affected by such changes. The incremental impact between 1.5 °C and 2 °C on high flows would be felt most by low income and lower middle income countries, the effect on soil moisture and low flows most by high income countries.
Publication Database... arrow_drop_down Fachrepositorium LebenswissenschaftenArticle . 2018License: CC BYData sources: Fachrepositorium LebenswissenschaftenPublikationsserver der Humboldt-Universität zu BerlinArticle . 2018 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu Berlinadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1088/1748-9326/aab792&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 77 citations 77 popularity Top 1% influence Top 10% impulse Top 1% Powered by BIP!
visibility 64visibility views 64 download downloads 31 Powered bymore_vert Publication Database... arrow_drop_down Fachrepositorium LebenswissenschaftenArticle . 2018License: CC BYData sources: Fachrepositorium LebenswissenschaftenPublikationsserver der Humboldt-Universität zu BerlinArticle . 2018 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu Berlinadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1088/1748-9326/aab792&type=result"></script>'); --> </script>
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description Publicationkeyboard_double_arrow_right Article , Journal , Research 2015 GermanyPublisher:IOP Publishing Dieter Gerten; Sibyll Schaphoff; Sebastian Ostberg; Wolfgang Lucht; Wolfgang Lucht;Human land use and anthropogenic climate change (CC) are placing mounting pressure on natural ecosystems worldwide, with impacts on biodiversity, water resources, nutrient and carbon cycles. Here, we present a quantitative macro-scale comparative analysis of the separate and joint dual impacts of land use and land cover change (LULCC) and CC on the terrestrial biosphere during the last ca. 300 years, based on simulations with a dynamic global vegetation model and an aggregated metric of simultaneous biogeochemical, hydrological and vegetation-structural shifts. We find that by the beginning of the 21st century LULCC and CC have jointly caused major shifts on more than 90% of all areas now cultivated, corresponding to 26% of the land area. CC has exposed another 26% of natural ecosystems to moderate or major shifts. Within three centuries, the impact of LULCC on landscapes has increased 13-fold. Within just one century, CC effects have caught up with LULCC effects.
Publication Database... arrow_drop_down Publikationsserver der Humboldt-Universität zu BerlinArticle . 2015 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu Berlinadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1088/1748-9326/10/4/044011&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 58 citations 58 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!
visibility 69visibility views 69 download downloads 51 Powered bymore_vert Publication Database... arrow_drop_down Publikationsserver der Humboldt-Universität zu BerlinArticle . 2015 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu Berlinadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Journal , Research 2015 GermanyPublisher:IOP Publishing Dieter Gerten; Sibyll Schaphoff; Sebastian Ostberg; Wolfgang Lucht; Wolfgang Lucht;Human land use and anthropogenic climate change (CC) are placing mounting pressure on natural ecosystems worldwide, with impacts on biodiversity, water resources, nutrient and carbon cycles. Here, we present a quantitative macro-scale comparative analysis of the separate and joint dual impacts of land use and land cover change (LULCC) and CC on the terrestrial biosphere during the last ca. 300 years, based on simulations with a dynamic global vegetation model and an aggregated metric of simultaneous biogeochemical, hydrological and vegetation-structural shifts. We find that by the beginning of the 21st century LULCC and CC have jointly caused major shifts on more than 90% of all areas now cultivated, corresponding to 26% of the land area. CC has exposed another 26% of natural ecosystems to moderate or major shifts. Within three centuries, the impact of LULCC on landscapes has increased 13-fold. Within just one century, CC effects have caught up with LULCC effects.
Publication Database... arrow_drop_down Publikationsserver der Humboldt-Universität zu BerlinArticle . 2015 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu Berlinadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1088/1748-9326/10/4/044011&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 58 citations 58 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!
visibility 69visibility views 69 download downloads 51 Powered bymore_vert Publication Database... arrow_drop_down Publikationsserver der Humboldt-Universität zu BerlinArticle . 2015 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu Berlinadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type , Journal 2017 France, United States, France, United Kingdom, United States, Germany, France, Sweden, Netherlands, Spain, Netherlands, United Kingdom, United States, NetherlandsPublisher:Copernicus GmbH Funded by:EC | SIM4NEXUS, EC | CD-LINKS, NWO | Multi-scale and self-cons... +6 projectsEC| SIM4NEXUS ,EC| CD-LINKS ,NWO| Multi-scale and self-consistent observations of recent sea level change ,EC| IMBALANCE-P ,EC| GREEN-WIN ,NSF| Collaborative Research: EaSM2--Wildfires and Regional Climate Variability - Mechanisms, Modeling, and Prediction ,EC| RISES-AM- ,EC| CRESCENDO ,EC| HELIXK. Frieler; S. Lange; F. Piontek; C. P. O. Reyer; J. Schewe; L. Warszawski; F. Zhao; L. Chini; S. Denvil; K. Emanuel; T. Geiger; K. Halladay; G. Hurtt; M. Mengel; D. Murakami; S. Ostberg; S. Ostberg; A. Popp; R. Riva; R. Riva; M. Stevanovic; T. Suzuki; J. Volkholz; E. Burke; P. Ciais; K. Ebi; T. D. Eddy; T. D. Eddy; J. Elliott; J. Elliott; E. Galbraith; E. Galbraith; S. N. Gosling; F. Hattermann; T. Hickler; J. Hinkel; J. Hinkel; C. Hof; V. Huber; J. Jägermeyr; V. Krysanova; R. Marcé; H. Müller Schmied; H. Müller Schmied; I. Mouratiadou; I. Mouratiadou; D. Pierson; D. P. Tittensor; D. P. Tittensor; R. Vautard; M. van Vliet; M. F. Biber; R. A. Betts; R. A. Betts; B. L. Bodirsky; D. Deryng; D. Deryng; S. Frolking; C. D. Jones; H. K. Lotze; H. Lotze-Campen; H. Lotze-Campen; R. Sahajpal; K. Thonicke; H. Tian; H. Tian; Y. Yamagata;handle: 1721.1/119493
Abstract. In Paris, France, December 2015, the Conference of the Parties (COP) to the United Nations Framework Convention on Climate Change (UNFCCC) invited the Intergovernmental Panel on Climate Change (IPCC) to provide a special report in 2018 on the impacts of global warming of 1.5 °C above pre-industrial levels and related global greenhouse gas emission pathways. In Nairobi, Kenya, April 2016, the IPCC panel accepted the invitation. Here we describe the response devised within the Inter-Sectoral Impact Model Intercomparison Project (ISIMIP) to provide tailored, cross-sectorally consistent impact projections to broaden the scientific basis for the report. The simulation protocol is designed to allow for (1) separation of the impacts of historical warming starting from pre-industrial conditions from impacts of other drivers such as historical land-use changes (based on pre-industrial and historical impact model simulations); (2) quantification of the impacts of additional warming up to 1.5 °C, including a potential overshoot and long-term impacts up to 2299, and comparison to higher levels of global mean temperature change (based on the low-emissions Representative Concentration Pathway RCP2.6 and a no-mitigation pathway RCP6.0) with socio-economic conditions fixed at 2005 levels; and (3) assessment of the climate effects based on the same climate scenarios while accounting for simultaneous changes in socio-economic conditions following the middle-of-the-road Shared Socioeconomic Pathway (SSP2, Fricko et al., 2016) and in particular differential bioenergy requirements associated with the transformation of the energy system to comply with RCP2.6 compared to RCP6.0. With the aim of providing the scientific basis for an aggregation of impacts across sectors and analysis of cross-sectoral interactions that may dampen or amplify sectoral impacts, the protocol is designed to facilitate consistent impact projections from a range of impact models across different sectors (global and regional hydrology, lakes, global crops, global vegetation, regional forests, global and regional marine ecosystems and fisheries, global and regional coastal infrastructure, energy supply and demand, temperature-related mortality, and global terrestrial biodiversity).
Nottingham Research ... arrow_drop_down University of New Hampshire: Scholars RepositoryArticle . 2017License: CC BYFull-Text: https://scholars.unh.edu/ersc/203Data sources: Bielefeld Academic Search Engine (BASE)DSpace@MIT (Massachusetts Institute of Technology)Article . 2017License: CC BYFull-Text: https://doi.org/10.5194/gmd-10-4321-2017Data sources: Bielefeld Academic Search Engine (BASE)Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2017License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2017Full-Text: https://hal.science/hal-02922298Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2017Full-Text: https://hal.science/hal-02922298Data sources: Bielefeld Academic Search Engine (BASE)Geoscientific Model DevelopmentArticle . 2017Data sources: DANS (Data Archiving and Networked Services)Geoscientific Model DevelopmentArticle . 2017Data sources: DANS (Data Archiving and Networked Services)Recolector de Ciencia Abierta, RECOLECTAArticle . 2017License: CC BYData sources: Recolector de Ciencia Abierta, RECOLECTADiposit Digital de Documents de la UABArticle . 2017License: CC BYData sources: Diposit Digital de Documents de la UABFachrepositorium LebenswissenschaftenArticle . 2017License: CC BYData sources: Fachrepositorium LebenswissenschaftenPublikationer från Uppsala UniversitetArticle . 2017Data sources: Publikationer från Uppsala UniversitetWageningen Staff PublicationsArticle . 2017License: CC BYData sources: Wageningen Staff PublicationsDigitala Vetenskapliga Arkivet - Academic Archive On-lineArticle . 2017 . Peer-reviewedGeoscientific Model DevelopmentArticle . 2017 . Peer-reviewedData sources: European Union Open Data PortalDelft University of Technology: Institutional RepositoryArticle . 2017Data sources: Bielefeld Academic Search Engine (BASE)Knowledge@UChicago (University of Chicago)Article . 2024Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 467 citations 467 popularity Top 0.1% influence Top 1% impulse Top 0.1% Powered by BIP!
visibility 6visibility views 6 download downloads 18 Powered bymore_vert Nottingham Research ... arrow_drop_down University of New Hampshire: Scholars RepositoryArticle . 2017License: CC BYFull-Text: https://scholars.unh.edu/ersc/203Data sources: Bielefeld Academic Search Engine (BASE)DSpace@MIT (Massachusetts Institute of Technology)Article . 2017License: CC BYFull-Text: https://doi.org/10.5194/gmd-10-4321-2017Data sources: Bielefeld Academic Search Engine (BASE)Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2017License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2017Full-Text: https://hal.science/hal-02922298Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2017Full-Text: https://hal.science/hal-02922298Data sources: Bielefeld Academic Search Engine (BASE)Geoscientific Model DevelopmentArticle . 2017Data sources: DANS (Data Archiving and Networked Services)Geoscientific Model DevelopmentArticle . 2017Data sources: DANS (Data Archiving and Networked Services)Recolector de Ciencia Abierta, RECOLECTAArticle . 2017License: CC BYData sources: Recolector de Ciencia Abierta, RECOLECTADiposit Digital de Documents de la UABArticle . 2017License: CC BYData sources: Diposit Digital de Documents de la UABFachrepositorium LebenswissenschaftenArticle . 2017License: CC BYData sources: Fachrepositorium LebenswissenschaftenPublikationer från Uppsala UniversitetArticle . 2017Data sources: Publikationer från Uppsala UniversitetWageningen Staff PublicationsArticle . 2017License: CC BYData sources: Wageningen Staff PublicationsDigitala Vetenskapliga Arkivet - Academic Archive On-lineArticle . 2017 . Peer-reviewedGeoscientific Model DevelopmentArticle . 2017 . Peer-reviewedData sources: European Union Open Data PortalDelft University of Technology: Institutional RepositoryArticle . 2017Data sources: Bielefeld Academic Search Engine (BASE)Knowledge@UChicago (University of Chicago)Article . 2024Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type , Journal 2017 France, United States, France, United Kingdom, United States, Germany, France, Sweden, Netherlands, Spain, Netherlands, United Kingdom, United States, NetherlandsPublisher:Copernicus GmbH Funded by:EC | SIM4NEXUS, EC | CD-LINKS, NWO | Multi-scale and self-cons... +6 projectsEC| SIM4NEXUS ,EC| CD-LINKS ,NWO| Multi-scale and self-consistent observations of recent sea level change ,EC| IMBALANCE-P ,EC| GREEN-WIN ,NSF| Collaborative Research: EaSM2--Wildfires and Regional Climate Variability - Mechanisms, Modeling, and Prediction ,EC| RISES-AM- ,EC| CRESCENDO ,EC| HELIXK. Frieler; S. Lange; F. Piontek; C. P. O. Reyer; J. Schewe; L. Warszawski; F. Zhao; L. Chini; S. Denvil; K. Emanuel; T. Geiger; K. Halladay; G. Hurtt; M. Mengel; D. Murakami; S. Ostberg; S. Ostberg; A. Popp; R. Riva; R. Riva; M. Stevanovic; T. Suzuki; J. Volkholz; E. Burke; P. Ciais; K. Ebi; T. D. Eddy; T. D. Eddy; J. Elliott; J. Elliott; E. Galbraith; E. Galbraith; S. N. Gosling; F. Hattermann; T. Hickler; J. Hinkel; J. Hinkel; C. Hof; V. Huber; J. Jägermeyr; V. Krysanova; R. Marcé; H. Müller Schmied; H. Müller Schmied; I. Mouratiadou; I. Mouratiadou; D. Pierson; D. P. Tittensor; D. P. Tittensor; R. Vautard; M. van Vliet; M. F. Biber; R. A. Betts; R. A. Betts; B. L. Bodirsky; D. Deryng; D. Deryng; S. Frolking; C. D. Jones; H. K. Lotze; H. Lotze-Campen; H. Lotze-Campen; R. Sahajpal; K. Thonicke; H. Tian; H. Tian; Y. Yamagata;handle: 1721.1/119493
Abstract. In Paris, France, December 2015, the Conference of the Parties (COP) to the United Nations Framework Convention on Climate Change (UNFCCC) invited the Intergovernmental Panel on Climate Change (IPCC) to provide a special report in 2018 on the impacts of global warming of 1.5 °C above pre-industrial levels and related global greenhouse gas emission pathways. In Nairobi, Kenya, April 2016, the IPCC panel accepted the invitation. Here we describe the response devised within the Inter-Sectoral Impact Model Intercomparison Project (ISIMIP) to provide tailored, cross-sectorally consistent impact projections to broaden the scientific basis for the report. The simulation protocol is designed to allow for (1) separation of the impacts of historical warming starting from pre-industrial conditions from impacts of other drivers such as historical land-use changes (based on pre-industrial and historical impact model simulations); (2) quantification of the impacts of additional warming up to 1.5 °C, including a potential overshoot and long-term impacts up to 2299, and comparison to higher levels of global mean temperature change (based on the low-emissions Representative Concentration Pathway RCP2.6 and a no-mitigation pathway RCP6.0) with socio-economic conditions fixed at 2005 levels; and (3) assessment of the climate effects based on the same climate scenarios while accounting for simultaneous changes in socio-economic conditions following the middle-of-the-road Shared Socioeconomic Pathway (SSP2, Fricko et al., 2016) and in particular differential bioenergy requirements associated with the transformation of the energy system to comply with RCP2.6 compared to RCP6.0. With the aim of providing the scientific basis for an aggregation of impacts across sectors and analysis of cross-sectoral interactions that may dampen or amplify sectoral impacts, the protocol is designed to facilitate consistent impact projections from a range of impact models across different sectors (global and regional hydrology, lakes, global crops, global vegetation, regional forests, global and regional marine ecosystems and fisheries, global and regional coastal infrastructure, energy supply and demand, temperature-related mortality, and global terrestrial biodiversity).
Nottingham Research ... arrow_drop_down University of New Hampshire: Scholars RepositoryArticle . 2017License: CC BYFull-Text: https://scholars.unh.edu/ersc/203Data sources: Bielefeld Academic Search Engine (BASE)DSpace@MIT (Massachusetts Institute of Technology)Article . 2017License: CC BYFull-Text: https://doi.org/10.5194/gmd-10-4321-2017Data sources: Bielefeld Academic Search Engine (BASE)Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2017License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2017Full-Text: https://hal.science/hal-02922298Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2017Full-Text: https://hal.science/hal-02922298Data sources: Bielefeld Academic Search Engine (BASE)Geoscientific Model DevelopmentArticle . 2017Data sources: DANS (Data Archiving and Networked Services)Geoscientific Model DevelopmentArticle . 2017Data sources: DANS (Data Archiving and Networked Services)Recolector de Ciencia Abierta, RECOLECTAArticle . 2017License: CC BYData sources: Recolector de Ciencia Abierta, RECOLECTADiposit Digital de Documents de la UABArticle . 2017License: CC BYData sources: Diposit Digital de Documents de la UABFachrepositorium LebenswissenschaftenArticle . 2017License: CC BYData sources: Fachrepositorium LebenswissenschaftenPublikationer från Uppsala UniversitetArticle . 2017Data sources: Publikationer från Uppsala UniversitetWageningen Staff PublicationsArticle . 2017License: CC BYData sources: Wageningen Staff PublicationsDigitala Vetenskapliga Arkivet - Academic Archive On-lineArticle . 2017 . Peer-reviewedGeoscientific Model DevelopmentArticle . 2017 . Peer-reviewedData sources: European Union Open Data PortalDelft University of Technology: Institutional RepositoryArticle . 2017Data sources: Bielefeld Academic Search Engine (BASE)Knowledge@UChicago (University of Chicago)Article . 2024Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 467 citations 467 popularity Top 0.1% influence Top 1% impulse Top 0.1% Powered by BIP!
visibility 6visibility views 6 download downloads 18 Powered bymore_vert Nottingham Research ... arrow_drop_down University of New Hampshire: Scholars RepositoryArticle . 2017License: CC BYFull-Text: https://scholars.unh.edu/ersc/203Data sources: Bielefeld Academic Search Engine (BASE)DSpace@MIT (Massachusetts Institute of Technology)Article . 2017License: CC BYFull-Text: https://doi.org/10.5194/gmd-10-4321-2017Data sources: Bielefeld Academic Search Engine (BASE)Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2017License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2017Full-Text: https://hal.science/hal-02922298Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2017Full-Text: https://hal.science/hal-02922298Data sources: Bielefeld Academic Search Engine (BASE)Geoscientific Model DevelopmentArticle . 2017Data sources: DANS (Data Archiving and Networked Services)Geoscientific Model DevelopmentArticle . 2017Data sources: DANS (Data Archiving and Networked Services)Recolector de Ciencia Abierta, RECOLECTAArticle . 2017License: CC BYData sources: Recolector de Ciencia Abierta, RECOLECTADiposit Digital de Documents de la UABArticle . 2017License: CC BYData sources: Diposit Digital de Documents de la UABFachrepositorium LebenswissenschaftenArticle . 2017License: CC BYData sources: Fachrepositorium LebenswissenschaftenPublikationer från Uppsala UniversitetArticle . 2017Data sources: Publikationer från Uppsala UniversitetWageningen Staff PublicationsArticle . 2017License: CC BYData sources: Wageningen Staff PublicationsDigitala Vetenskapliga Arkivet - Academic Archive On-lineArticle . 2017 . Peer-reviewedGeoscientific Model DevelopmentArticle . 2017 . Peer-reviewedData sources: European Union Open Data PortalDelft University of Technology: Institutional RepositoryArticle . 2017Data sources: Bielefeld Academic Search Engine (BASE)Knowledge@UChicago (University of Chicago)Article . 2024Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Conference object , Other literature type , Journal 2017 France, France, France, France, France, France, Germany, FrancePublisher:IOP Publishing Funded by:EC | IMBALANCE-P, NSF | Collaborative Research: E..., EC | HELIXEC| IMBALANCE-P ,NSF| Collaborative Research: EaSM2--Wildfires and Regional Climate Variability - Mechanisms, Modeling, and Prediction ,EC| HELIXAuthors: Sibyll Schaphoff; Christopher P. O. Reyer; Frédéric Chevallier; Jörg Steinkamp; +29 AuthorsSibyll Schaphoff; Christopher P. O. Reyer; Frédéric Chevallier; Jörg Steinkamp; Jia Yang; Rashid Rafique; Ghassem R. Asrar; Ning Zeng; Kazuya Nishina; Akihiko Ito; Shushi Peng; Fang Zhao; Shufen Pan; Sebastian Ostberg; Sebastian Ostberg; Jinfeng Chang; Jinfeng Chang; Louis François; Shilong Piao; Katja Frieler; Guy Munhoven; Marie Dury; Thomas Hickler; Philippe Ciais; Xuhui Wang; Xuhui Wang; Alexandra-Jane Henrot; Hanqin Tian; Christrian Rödenbeck; Anselmo Garcia Cantu Ros; Richard Betts; Nicolas Viovy; Catherine Morfopoulos;Le but de cette étude est d'évaluer les huit modèles de biome ISIMIP2a par rapport à des estimations indépendantes des flux nets de carbone à long terme (c'est-à-dire la productivité nette du biome, NBP) sur les écosystèmes terrestres au cours des quatre dernières décennies (1971–2010). Nous évaluons le NBP mondial modélisé par rapport à 1) le puits terrestre résiduel mondial (RLS) mis à jour plus les émissions liées à l'utilisation des terres (ELUC) du Global Carbon Project (GCP), présenté comme R + L dans cette étude par Le Quéré et al (2015), et 2) les flux de CO2 terrestre provenant de deux systèmes d'inversion atmosphérique : Jena CarboScope s81_v3.8 et CAMS v15r2, appelés FJena et FCAMS respectivement. L'ensemble de modèles - moyenne NBP (qui comprend sept modèles avec changement d'affectation des terres) est plus élevé que mais dans l'incertitude de R + L, tandis que la tendance NBP positive simulée au cours des 30 dernières années est inférieure à celle de R + L et des deux systèmes d'inversion. Les modèles de biome ISIMIP2a capturent bien la variation interannuelle des flux nets mondiaux de carbone des écosystèmes terrestres. La NBP tropicale représente 31 ± 17 % de la NBP totale mondiale au cours des dernières décennies, et la variation d'une année à l'autre de la NBP tropicale contribue pour l'essentiel à la variation interannuelle de la NBP mondiale. Selon les modèles, l'augmentation de la productivité primaire nette (NPP) a été la principale cause de l'augmentation générale de la NBP. Des anomalies NBP globales significatives à partir de la moyenne à long terme entre les deux phases des événements El Niño Southern Oscillation (ENSO) sont simulées par tous les modèles (p < 0,05), ce qui est cohérent avec l'estimation R + L (p = 0,06), également principalement attribuée à des anomalies NPP, plutôt qu'à des changements dans la respiration hétérotrophique (Rh). Les anomalies mondiales de la centrale nucléaire et de la centrale nucléaire nucléaire pendant les événements ENSO sont dominées par leurs anomalies dans les régions tropicales touchées par la variabilité du climat tropical. Les régressions multiples entre les variations interannuelles de R + L, FJena et FCAMS et les variations du climat tropical révèlent une réponse négative significative des flux nets mondiaux de carbone des écosystèmes terrestres à la variation de la température annuelle moyenne tropicale, et une réponse non significative à la variation des précipitations annuelles tropicales. Selon les modèles, les précipitations tropicales sont un facteur plus important, ce qui suggère que certains modèles ne saisissent pas correctement les rôles des précipitations et des changements de température. El propósito de este estudio es evaluar los ocho modelos de bioma ISIMIP2a contra estimaciones independientes de flujos netos de carbono a largo plazo (es decir, Productividad Neta del Bioma, NBP) sobre ecosistemas terrestres durante las últimas cuatro décadas (1971–2010). Evaluamos el NBP global modelado contra 1) el sumidero de tierra residual (RLS) global actualizado más las emisiones de uso de la tierra (ELUC) del Proyecto Global de Carbono (GCP), presentado como R + L en este estudio por Le Quéré et al (2015), y 2) los flujos de CO2 terrestre de dos sistemas de inversión atmosférica: Jena CarboScope s81_v3.8 y CAMS v15r2, denominados FJena y FCAMS respectivamente. La media del conjunto de modelos NBP (que incluye siete modelos con cambio de uso de la tierra) es mayor que, pero dentro de la incertidumbre de R + L, mientras que la tendencia positiva simulada de NBP en los últimos 30 años es menor que la de R + L y de los dos sistemas de inversión. Los modelos de bioma ISIMIP2a capturan bien la variación interanual de los flujos netos globales de carbono del ecosistema terrestre. El NBP tropical representa el 31 ± 17% del NBP total global durante las últimas décadas, y la variación interanual del NBP tropical contribuye con la mayor parte de la variación interanual del NBP global. Según los modelos, el aumento de la productividad primaria neta (PPN) fue la causa principal del aumento general de la PNB. Todos los modelos simulan anomalías de NBP globales significativas de la media a largo plazo entre las dos fases de los eventos de El Niño Oscilación del Sur (Enos) (p < 0.05), lo cual es consistente con la estimación de R + L (p = 0.06), también atribuida principalmente a anomalías de NPP, más que a cambios en la respiración heterótrofa (Rh). Las anomalías globales de NPP y NBP durante los eventos Enos están dominadas por sus anomalías en las regiones tropicales afectadas por la variabilidad del clima tropical. Las múltiples regresiones entre las variaciones interanuales de R + L, FJena y FCAMS y las variaciones del clima tropical revelan una respuesta negativa significativa de los flujos netos globales de carbono del ecosistema terrestre a la variación de la temperatura media anual tropical, y una respuesta no significativa a la variación de la precipitación anual tropical. Según los modelos, la precipitación tropical es un impulsor más importante, lo que sugiere que algunos modelos no capturan adecuadamente los roles de la precipitación y los cambios de temperatura. The purpose of this study is to evaluate the eight ISIMIP2a biome models against independent estimates of long-term net carbon fluxes (i.e. Net Biome Productivity, NBP) over terrestrial ecosystems for the recent four decades (1971–2010). We evaluate modeled global NBP against 1) the updated global residual land sink (RLS) plus land use emissions (ELUC) from the Global Carbon Project (GCP), presented as R + L in this study by Le Quéré et al (2015), and 2) the land CO2 fluxes from two atmospheric inversion systems: Jena CarboScope s81_v3.8 and CAMS v15r2, referred to as FJena and FCAMS respectively. The model ensemble-mean NBP (that includes seven models with land-use change) is higher than but within the uncertainty of R + L, while the simulated positive NBP trend over the last 30 yr is lower than that from R + L and from the two inversion systems. ISIMIP2a biome models well capture the interannual variation of global net terrestrial ecosystem carbon fluxes. Tropical NBP represents 31 ± 17% of global total NBP during the past decades, and the year-to-year variation of tropical NBP contributes most of the interannual variation of global NBP. According to the models, increasing Net Primary Productivity (NPP) was the main cause for the generally increasing NBP. Significant global NBP anomalies from the long-term mean between the two phases of El Niño Southern Oscillation (ENSO) events are simulated by all models (p < 0.05), which is consistent with the R + L estimate (p = 0.06), also mainly attributed to NPP anomalies, rather than to changes in heterotrophic respiration (Rh). The global NPP and NBP anomalies during ENSO events are dominated by their anomalies in tropical regions impacted by tropical climate variability. Multiple regressions between R + L, FJena and FCAMS interannual variations and tropical climate variations reveal a significant negative response of global net terrestrial ecosystem carbon fluxes to tropical mean annual temperature variation, and a non-significant response to tropical annual precipitation variation. According to the models, tropical precipitation is a more important driver, suggesting that some models do not capture the roles of precipitation and temperature changes adequately. الغرض من هذه الدراسة هو تقييم نماذج المناطق الأحيائية الثمانية ISIMIP2a مقابل التقديرات المستقلة لصافي تدفقات الكربون طويلة الأجل (أي صافي إنتاجية المناطق الأحيائية) على النظم الإيكولوجية الأرضية على مدى العقود الأربعة الأخيرة (1971–2010). نقوم بتقييم خطة العمل الوطنية العالمية المنمذجة مقابل 1) بالوعة الأراضي المتبقية العالمية المحدثة بالإضافة إلى انبعاثات استخدام الأراضي (ELUC) من مشروع الكربون العالمي (GCP)، والتي تم تقديمها على أنها R + L في هذه الدراسة من قبل Le Quéré et al (2015)، و 2) تدفقات ثاني أكسيد الكربون الأرضية من نظامين لعكس الغلاف الجوي: Jena CarboScope s81_v3.8 و CAMS v15r2، المشار إليها باسم FJena و FCAMS على التوالي. إن مجموعة النماذج - تعني NBP (التي تتضمن سبعة نماذج مع تغيير استخدام الأراضي) أعلى من ولكن ضمن عدم اليقين من R + L، في حين أن اتجاه NBP الإيجابي المحاكي على مدار الثلاثين عامًا الماضية أقل من ذلك من R + L ومن نظامي الانعكاس. تلتقط نماذج المناطق الأحيائية ISIMIP2a بشكل جيد التباين السنوي لتدفقات الكربون الصافية للنظام الإيكولوجي الأرضي العالمي. يمثل الناتج القومي الاستوائي 31 ± 17 ٪ من إجمالي الناتج القومي العالمي خلال العقود الماضية، ويساهم التباين من سنة إلى أخرى في الناتج القومي الاستوائي في معظم التباين السنوي في الناتج القومي العالمي. وفقًا للنماذج، كانت زيادة صافي الإنتاجية الأولية هي السبب الرئيسي لزيادة صافي الإنتاجية الأولية بشكل عام. تتم محاكاة حالات الشذوذ العالمية الكبيرة من المتوسط طويل الأجل بين مرحلتي أحداث التذبذب الجنوبي لظاهرة النينيو (ENSO) من خلال جميع النماذج (P < 0.05)، وهو ما يتوافق مع تقدير R + L (P = 0.06)، والذي يعزى أيضًا بشكل أساسي إلى حالات الشذوذ في NPP، بدلاً من التغيرات في التنفس غيري التغذية (Rh). تهيمن الشذوذات العالمية لمحطات الطاقة النووية ومحطات الطاقة الوطنية خلال أحداث ENSO على شذوذاتها في المناطق المدارية المتأثرة بتقلب المناخ المداري. تكشف الانحدارات المتعددة بين الاختلافات السنوية بين R + L و FJENA و FCAMS والتغيرات المناخية المدارية عن استجابة سلبية كبيرة لصافي تدفقات الكربون في النظام الإيكولوجي الأرضي العالمي لمتوسط التغير السنوي في درجة الحرارة المدارية، واستجابة غير كبيرة لتغير هطول الأمطار السنوي المداري. وفقًا للنماذج، يعد هطول الأمطار الاستوائية محركًا أكثر أهمية، مما يشير إلى أن بعض النماذج لا تلتقط أدوار هطول الأمطار وتغيرات درجة الحرارة بشكل كافٍ.
Hyper Article en Lig... arrow_drop_down École Polytechnique, Université Paris-Saclay: HALArticle . 2017Full-Text: https://hal.science/hal-01828297Data sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2017Full-Text: https://hal.science/hal-01828297Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2017Full-Text: https://hal.science/hal-01828297Data sources: Bielefeld Academic Search Engine (BASE)Fachrepositorium LebenswissenschaftenArticle . 2017License: CC BYData sources: Fachrepositorium Lebenswissenschaftenhttp://dx.doi.org/https://iops...Other literature typeData sources: European Union Open Data Portaladd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 34 citations 34 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Conference object , Other literature type , Journal 2017 France, France, France, France, France, France, Germany, FrancePublisher:IOP Publishing Funded by:EC | IMBALANCE-P, NSF | Collaborative Research: E..., EC | HELIXEC| IMBALANCE-P ,NSF| Collaborative Research: EaSM2--Wildfires and Regional Climate Variability - Mechanisms, Modeling, and Prediction ,EC| HELIXAuthors: Sibyll Schaphoff; Christopher P. O. Reyer; Frédéric Chevallier; Jörg Steinkamp; +29 AuthorsSibyll Schaphoff; Christopher P. O. Reyer; Frédéric Chevallier; Jörg Steinkamp; Jia Yang; Rashid Rafique; Ghassem R. Asrar; Ning Zeng; Kazuya Nishina; Akihiko Ito; Shushi Peng; Fang Zhao; Shufen Pan; Sebastian Ostberg; Sebastian Ostberg; Jinfeng Chang; Jinfeng Chang; Louis François; Shilong Piao; Katja Frieler; Guy Munhoven; Marie Dury; Thomas Hickler; Philippe Ciais; Xuhui Wang; Xuhui Wang; Alexandra-Jane Henrot; Hanqin Tian; Christrian Rödenbeck; Anselmo Garcia Cantu Ros; Richard Betts; Nicolas Viovy; Catherine Morfopoulos;Le but de cette étude est d'évaluer les huit modèles de biome ISIMIP2a par rapport à des estimations indépendantes des flux nets de carbone à long terme (c'est-à-dire la productivité nette du biome, NBP) sur les écosystèmes terrestres au cours des quatre dernières décennies (1971–2010). Nous évaluons le NBP mondial modélisé par rapport à 1) le puits terrestre résiduel mondial (RLS) mis à jour plus les émissions liées à l'utilisation des terres (ELUC) du Global Carbon Project (GCP), présenté comme R + L dans cette étude par Le Quéré et al (2015), et 2) les flux de CO2 terrestre provenant de deux systèmes d'inversion atmosphérique : Jena CarboScope s81_v3.8 et CAMS v15r2, appelés FJena et FCAMS respectivement. L'ensemble de modèles - moyenne NBP (qui comprend sept modèles avec changement d'affectation des terres) est plus élevé que mais dans l'incertitude de R + L, tandis que la tendance NBP positive simulée au cours des 30 dernières années est inférieure à celle de R + L et des deux systèmes d'inversion. Les modèles de biome ISIMIP2a capturent bien la variation interannuelle des flux nets mondiaux de carbone des écosystèmes terrestres. La NBP tropicale représente 31 ± 17 % de la NBP totale mondiale au cours des dernières décennies, et la variation d'une année à l'autre de la NBP tropicale contribue pour l'essentiel à la variation interannuelle de la NBP mondiale. Selon les modèles, l'augmentation de la productivité primaire nette (NPP) a été la principale cause de l'augmentation générale de la NBP. Des anomalies NBP globales significatives à partir de la moyenne à long terme entre les deux phases des événements El Niño Southern Oscillation (ENSO) sont simulées par tous les modèles (p < 0,05), ce qui est cohérent avec l'estimation R + L (p = 0,06), également principalement attribuée à des anomalies NPP, plutôt qu'à des changements dans la respiration hétérotrophique (Rh). Les anomalies mondiales de la centrale nucléaire et de la centrale nucléaire nucléaire pendant les événements ENSO sont dominées par leurs anomalies dans les régions tropicales touchées par la variabilité du climat tropical. Les régressions multiples entre les variations interannuelles de R + L, FJena et FCAMS et les variations du climat tropical révèlent une réponse négative significative des flux nets mondiaux de carbone des écosystèmes terrestres à la variation de la température annuelle moyenne tropicale, et une réponse non significative à la variation des précipitations annuelles tropicales. Selon les modèles, les précipitations tropicales sont un facteur plus important, ce qui suggère que certains modèles ne saisissent pas correctement les rôles des précipitations et des changements de température. El propósito de este estudio es evaluar los ocho modelos de bioma ISIMIP2a contra estimaciones independientes de flujos netos de carbono a largo plazo (es decir, Productividad Neta del Bioma, NBP) sobre ecosistemas terrestres durante las últimas cuatro décadas (1971–2010). Evaluamos el NBP global modelado contra 1) el sumidero de tierra residual (RLS) global actualizado más las emisiones de uso de la tierra (ELUC) del Proyecto Global de Carbono (GCP), presentado como R + L en este estudio por Le Quéré et al (2015), y 2) los flujos de CO2 terrestre de dos sistemas de inversión atmosférica: Jena CarboScope s81_v3.8 y CAMS v15r2, denominados FJena y FCAMS respectivamente. La media del conjunto de modelos NBP (que incluye siete modelos con cambio de uso de la tierra) es mayor que, pero dentro de la incertidumbre de R + L, mientras que la tendencia positiva simulada de NBP en los últimos 30 años es menor que la de R + L y de los dos sistemas de inversión. Los modelos de bioma ISIMIP2a capturan bien la variación interanual de los flujos netos globales de carbono del ecosistema terrestre. El NBP tropical representa el 31 ± 17% del NBP total global durante las últimas décadas, y la variación interanual del NBP tropical contribuye con la mayor parte de la variación interanual del NBP global. Según los modelos, el aumento de la productividad primaria neta (PPN) fue la causa principal del aumento general de la PNB. Todos los modelos simulan anomalías de NBP globales significativas de la media a largo plazo entre las dos fases de los eventos de El Niño Oscilación del Sur (Enos) (p < 0.05), lo cual es consistente con la estimación de R + L (p = 0.06), también atribuida principalmente a anomalías de NPP, más que a cambios en la respiración heterótrofa (Rh). Las anomalías globales de NPP y NBP durante los eventos Enos están dominadas por sus anomalías en las regiones tropicales afectadas por la variabilidad del clima tropical. Las múltiples regresiones entre las variaciones interanuales de R + L, FJena y FCAMS y las variaciones del clima tropical revelan una respuesta negativa significativa de los flujos netos globales de carbono del ecosistema terrestre a la variación de la temperatura media anual tropical, y una respuesta no significativa a la variación de la precipitación anual tropical. Según los modelos, la precipitación tropical es un impulsor más importante, lo que sugiere que algunos modelos no capturan adecuadamente los roles de la precipitación y los cambios de temperatura. The purpose of this study is to evaluate the eight ISIMIP2a biome models against independent estimates of long-term net carbon fluxes (i.e. Net Biome Productivity, NBP) over terrestrial ecosystems for the recent four decades (1971–2010). We evaluate modeled global NBP against 1) the updated global residual land sink (RLS) plus land use emissions (ELUC) from the Global Carbon Project (GCP), presented as R + L in this study by Le Quéré et al (2015), and 2) the land CO2 fluxes from two atmospheric inversion systems: Jena CarboScope s81_v3.8 and CAMS v15r2, referred to as FJena and FCAMS respectively. The model ensemble-mean NBP (that includes seven models with land-use change) is higher than but within the uncertainty of R + L, while the simulated positive NBP trend over the last 30 yr is lower than that from R + L and from the two inversion systems. ISIMIP2a biome models well capture the interannual variation of global net terrestrial ecosystem carbon fluxes. Tropical NBP represents 31 ± 17% of global total NBP during the past decades, and the year-to-year variation of tropical NBP contributes most of the interannual variation of global NBP. According to the models, increasing Net Primary Productivity (NPP) was the main cause for the generally increasing NBP. Significant global NBP anomalies from the long-term mean between the two phases of El Niño Southern Oscillation (ENSO) events are simulated by all models (p < 0.05), which is consistent with the R + L estimate (p = 0.06), also mainly attributed to NPP anomalies, rather than to changes in heterotrophic respiration (Rh). The global NPP and NBP anomalies during ENSO events are dominated by their anomalies in tropical regions impacted by tropical climate variability. Multiple regressions between R + L, FJena and FCAMS interannual variations and tropical climate variations reveal a significant negative response of global net terrestrial ecosystem carbon fluxes to tropical mean annual temperature variation, and a non-significant response to tropical annual precipitation variation. According to the models, tropical precipitation is a more important driver, suggesting that some models do not capture the roles of precipitation and temperature changes adequately. الغرض من هذه الدراسة هو تقييم نماذج المناطق الأحيائية الثمانية ISIMIP2a مقابل التقديرات المستقلة لصافي تدفقات الكربون طويلة الأجل (أي صافي إنتاجية المناطق الأحيائية) على النظم الإيكولوجية الأرضية على مدى العقود الأربعة الأخيرة (1971–2010). نقوم بتقييم خطة العمل الوطنية العالمية المنمذجة مقابل 1) بالوعة الأراضي المتبقية العالمية المحدثة بالإضافة إلى انبعاثات استخدام الأراضي (ELUC) من مشروع الكربون العالمي (GCP)، والتي تم تقديمها على أنها R + L في هذه الدراسة من قبل Le Quéré et al (2015)، و 2) تدفقات ثاني أكسيد الكربون الأرضية من نظامين لعكس الغلاف الجوي: Jena CarboScope s81_v3.8 و CAMS v15r2، المشار إليها باسم FJena و FCAMS على التوالي. إن مجموعة النماذج - تعني NBP (التي تتضمن سبعة نماذج مع تغيير استخدام الأراضي) أعلى من ولكن ضمن عدم اليقين من R + L، في حين أن اتجاه NBP الإيجابي المحاكي على مدار الثلاثين عامًا الماضية أقل من ذلك من R + L ومن نظامي الانعكاس. تلتقط نماذج المناطق الأحيائية ISIMIP2a بشكل جيد التباين السنوي لتدفقات الكربون الصافية للنظام الإيكولوجي الأرضي العالمي. يمثل الناتج القومي الاستوائي 31 ± 17 ٪ من إجمالي الناتج القومي العالمي خلال العقود الماضية، ويساهم التباين من سنة إلى أخرى في الناتج القومي الاستوائي في معظم التباين السنوي في الناتج القومي العالمي. وفقًا للنماذج، كانت زيادة صافي الإنتاجية الأولية هي السبب الرئيسي لزيادة صافي الإنتاجية الأولية بشكل عام. تتم محاكاة حالات الشذوذ العالمية الكبيرة من المتوسط طويل الأجل بين مرحلتي أحداث التذبذب الجنوبي لظاهرة النينيو (ENSO) من خلال جميع النماذج (P < 0.05)، وهو ما يتوافق مع تقدير R + L (P = 0.06)، والذي يعزى أيضًا بشكل أساسي إلى حالات الشذوذ في NPP، بدلاً من التغيرات في التنفس غيري التغذية (Rh). تهيمن الشذوذات العالمية لمحطات الطاقة النووية ومحطات الطاقة الوطنية خلال أحداث ENSO على شذوذاتها في المناطق المدارية المتأثرة بتقلب المناخ المداري. تكشف الانحدارات المتعددة بين الاختلافات السنوية بين R + L و FJENA و FCAMS والتغيرات المناخية المدارية عن استجابة سلبية كبيرة لصافي تدفقات الكربون في النظام الإيكولوجي الأرضي العالمي لمتوسط التغير السنوي في درجة الحرارة المدارية، واستجابة غير كبيرة لتغير هطول الأمطار السنوي المداري. وفقًا للنماذج، يعد هطول الأمطار الاستوائية محركًا أكثر أهمية، مما يشير إلى أن بعض النماذج لا تلتقط أدوار هطول الأمطار وتغيرات درجة الحرارة بشكل كافٍ.
Hyper Article en Lig... arrow_drop_down École Polytechnique, Université Paris-Saclay: HALArticle . 2017Full-Text: https://hal.science/hal-01828297Data sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2017Full-Text: https://hal.science/hal-01828297Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2017Full-Text: https://hal.science/hal-01828297Data sources: Bielefeld Academic Search Engine (BASE)Fachrepositorium LebenswissenschaftenArticle . 2017License: CC BYData sources: Fachrepositorium Lebenswissenschaftenhttp://dx.doi.org/https://iops...Other literature typeData sources: European Union Open Data Portaladd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 34 citations 34 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!
more_vert Hyper Article en Lig... arrow_drop_down École Polytechnique, Université Paris-Saclay: HALArticle . 2017Full-Text: https://hal.science/hal-01828297Data sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2017Full-Text: https://hal.science/hal-01828297Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2017Full-Text: https://hal.science/hal-01828297Data sources: Bielefeld Academic Search Engine (BASE)Fachrepositorium LebenswissenschaftenArticle . 2017License: CC BYData sources: Fachrepositorium Lebenswissenschaftenhttp://dx.doi.org/https://iops...Other literature typeData sources: European Union Open Data Portaladd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2024 Italy, GermanyPublisher:IOP Publishing Lisa Murken; Julia Tomalka; David Abigaba; Antwi-Bosiako Amoah; Joseph Armathé Amougou; Muriel Anaba; Ponraj Arumugam; Eres Awori; Hye-Rin Léa Baek; Till Below; Matti Cartsburg; Abel Chemura; Carla Cronauer; Iulii Didovets; Adefires Worku Gizaw; Stephanie Gleixner; Nele Gloy; Enrico Grams; Lemlem Habtemariam; Anna Hampf; Ylva Hauf; Tim Heckmann; Boubacar Ibrahim; Lennart Jansen; Francis Jarawura; Timothée Kagonbé; Juliane Kaufmann; Priscilla Kephe; Lena Klockemann; Stefan Lange; Rahel Laudien; Stefan Liersch; Naima Lipka; Sophia Lüttringhaus; Sibylla Neer; Oblé Neya; Steffen Noleppa; Sebastian Ostberg; Jonas Pollig; Paula Romanovska; Felicitas Röhrig; Bernhard Schauberger; Roopam Shukla; Lina Staubach; Mesmin Tchindjang; Sabine Undorf; Regina Vetter; Sophie von Loeben; Christoph von Stechow; Katarina von Witzke; Chiara Sophia Weituschat; Michel Wortmann; Amsalu Woldie Yalew; Isabella Zouh; Christoph Gornott;handle: 10278/5060923
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Environmental Resear... arrow_drop_down Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2024License: CC BYData sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 0 citations 0 popularity Average influence Average impulse Average Powered by BIP!
more_vert Environmental Resear... arrow_drop_down Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2024License: CC BYData sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2024 Italy, GermanyPublisher:IOP Publishing Lisa Murken; Julia Tomalka; David Abigaba; Antwi-Bosiako Amoah; Joseph Armathé Amougou; Muriel Anaba; Ponraj Arumugam; Eres Awori; Hye-Rin Léa Baek; Till Below; Matti Cartsburg; Abel Chemura; Carla Cronauer; Iulii Didovets; Adefires Worku Gizaw; Stephanie Gleixner; Nele Gloy; Enrico Grams; Lemlem Habtemariam; Anna Hampf; Ylva Hauf; Tim Heckmann; Boubacar Ibrahim; Lennart Jansen; Francis Jarawura; Timothée Kagonbé; Juliane Kaufmann; Priscilla Kephe; Lena Klockemann; Stefan Lange; Rahel Laudien; Stefan Liersch; Naima Lipka; Sophia Lüttringhaus; Sibylla Neer; Oblé Neya; Steffen Noleppa; Sebastian Ostberg; Jonas Pollig; Paula Romanovska; Felicitas Röhrig; Bernhard Schauberger; Roopam Shukla; Lina Staubach; Mesmin Tchindjang; Sabine Undorf; Regina Vetter; Sophie von Loeben; Christoph von Stechow; Katarina von Witzke; Chiara Sophia Weituschat; Michel Wortmann; Amsalu Woldie Yalew; Isabella Zouh; Christoph Gornott;handle: 10278/5060923
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Environmental Resear... arrow_drop_down Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2024License: CC BYData sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 0 citations 0 popularity Average influence Average impulse Average Powered by BIP!
more_vert Environmental Resear... arrow_drop_down Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2024License: CC BYData sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type , Journal , Research 2013 Germany, France, United Kingdom, FrancePublisher:IOP Publishing Funded by:EC | ERMITAGEEC| ERMITAGEGerten, Dieter; Lucht, Wolfgang; Ostberg, Sebastian; Heinke, Jens; Kowarsch, Martin; Kreft, Holger; Kundzewicz, Zbigniew W.; Rastgooy, Johann; Warren, Rachel; Schellnhuber, Hans Joachim; Gerten, Dieter;; Lucht, Wolfgang;; Ostberg, Sebastian;; Heinke, Jens;; Kowarsch, Martin;; Kreft, Holger;; Kundzewicz, Zbigniew W;; Rastgooy, Johann;; Warren, Rachel;; Schellnhuber, Hans Joachim;;handle: 10568/34462
Cette étude de modélisation démontre à quel niveau d'élévation de la température moyenne mondiale (ΔTg) les régions seront exposées à des diminutions significatives de la disponibilité en eau douce et à des changements dans les écosystèmes terrestres. Les projections sont basées sur un nouvel ensemble cohérent de 152 scénarios climatiques (huit trajectoires ΔTg atteignant 1,5-5 ° C au-dessus des niveaux préindustriels d'ici 2100, chacune mise à l'échelle avec des schémas spatiaux de 19 modèles de circulation générale). Les résultats suggèrent que déjà à un ΔTg de 2 ° C et principalement dans les régions subtropicales, une pénurie d'eau plus élevée se produirait dans plus de 50% des 19 scénarios climatiques. D'importants changements biogéochimiques et structurels de la végétation se produiraient également à 2 ° C, mais principalement dans les écosystèmes subpolaires et semi-arides. D'autres régions seraient affectées à des niveaux de ΔTg plus élevés, avec une intensité plus faible ou avec une confiance plus faible. Au total, des niveaux moyens de réchauffement planétaire de 2 ° C, 3,5 ° C et 5 ° C sont simulés pour exposer 8%, 11% et 13% supplémentaires de la population mondiale à une pénurie d'eau nouvelle ou aggravée, respectivement, avec une confiance >50% (alors qu'environ1,3 milliard de personnes vivent déjà dans des régions pauvres en eau). Parallèlement, des transformations substantielles de l'habitat se produiraient dans les régions biogéographiques qui contiennent 1% (dans les zones touchées à 2 ° C), 10% (3,5 ° C) et 74% (5 ° C) des espèces de plantes vasculaires actuelles pondérées par l'endémisme, respectivement. Les résultats suggèrent une croissance non linéaire des impacts avec ΔTg et mettent en évidence les disparités régionales dans les amplitudes d'impact et les niveaux critiques de ΔTg. Este estudio de modelado demuestra a qué nivel de aumento de la temperatura media global (ΔTg) las regiones estarán expuestas a disminuciones significativas de la disponibilidad de agua dulce y cambios en los ecosistemas terrestres. Las proyecciones se basan en un nuevo conjunto consistente de 152 escenarios climáticos (ocho trayectorias de ΔTg que alcanzan 1.5–5 ° C por encima de los niveles preindustriales para 2100, cada una escalada con patrones espaciales de 19 modelos de circulación general). Los resultados sugieren que ya a una ΔTg de 2°C y principalmente en los subtrópicos, se produciría una mayor escasez de agua en >50% de los 19 escenarios climáticos. También se producirían cambios estructurales sustanciales biogeoquímicos y de vegetación a 2 ° C, pero principalmente en ecosistemas subpolares y semiáridos. Otras regiones se verían afectadas a niveles más altos de ΔTg, con menor intensidad o con menor confianza. En total, se simulan niveles medios de calentamiento global de 2 ° C, 3,5 ° C y 5 ° C para exponer a un 8%, 11% y 13% adicionales de la población mundial a una escasez de agua nueva o agravada, respectivamente, con >50% de confianza (mientras que ~1.300 millones de personas ya viven en regiones con escasez de agua). Al mismo tiempo, se producirían transformaciones sustanciales del hábitat en regiones biogeográficas que contienen el 1% (en zonas afectadas a 2 ° C), el 10% (3.5 ° C) y el 74% (5 ° C) de las especies de plantas vasculares ponderadas por endemismo actuales, respectivamente. Los resultados sugieren un crecimiento no lineal de los impactos junto con ΔTg y resaltan las disparidades regionales en las magnitudes de impacto y los niveles críticos de ΔTg. This modelling study demonstrates at what level of global mean temperature rise (ΔTg) regions will be exposed to significant decreases of freshwater availability and changes to terrestrial ecosystems. Projections are based on a new, consistent set of 152 climate scenarios (eight ΔTg trajectories reaching 1.5–5 ° C above pre-industrial levels by 2100, each scaled with spatial patterns from 19 general circulation models). The results suggest that already at a ΔTg of 2 ° C and mainly in the subtropics, higher water scarcity would occur in >50% out of the 19 climate scenarios. Substantial biogeochemical and vegetation structural changes would also occur at 2 ° C, but mainly in subpolar and semiarid ecosystems. Other regions would be affected at higher ΔTg levels, with lower intensity or with lower confidence. In total, mean global warming levels of 2 ° C, 3.5 ° C and 5 ° C are simulated to expose an additional 8%, 11% and 13% of the world population to new or aggravated water scarcity, respectively, with >50% confidence (while ∼1.3 billion people already live in water-scarce regions). Concurrently, substantial habitat transformations would occur in biogeographic regions that contain 1% (in zones affected at 2 ° C), 10% (3.5 ° C) and 74% (5 ° C) of present endemism-weighted vascular plant species, respectively. The results suggest nonlinear growth of impacts along with ΔTg and highlight regional disparities in impact magnitudes and critical ΔTg levels. توضح دراسة النمذجة هذه مستوى مناطق متوسط ارتفاع درجة الحرارة العالمية (ΔTg) التي ستتعرض لانخفاضات كبيرة في توافر المياه العذبة والتغيرات في النظم الإيكولوجية الأرضية. تستند التوقعات إلى مجموعة جديدة ومتسقة من 152 سيناريو مناخيًا (ثمانية مسارات ΔTg تصل إلى 1.5–5 درجة مئوية فوق مستويات ما قبل الصناعة بحلول عام 2100، تم قياس كل منها بأنماط مكانية من 19 نموذج دوران عام). تشير النتائج إلى أنه بالفعل عند درجة حرارة 2 درجة مئوية وبشكل أساسي في المناطق شبه الاستوائية، ستحدث ندرة مياه أعلى في أكثر من 50 ٪ من السيناريوهات المناخية التسعة عشر. كما ستحدث تغييرات هيكلية بيوكيميائية ونباتية كبيرة عند 2 درجة مئوية، ولكن بشكل أساسي في النظم الإيكولوجية تحت القطبية وشبه القاحلة. ستتأثر المناطق الأخرى عند مستويات ΔTg أعلى، بكثافة أقل أو بثقة أقل. في المجموع، تتم محاكاة متوسط مستويات الاحترار العالمي البالغة 2 درجة مئوية و 3.5 درجة مئوية و 5 درجات مئوية لتعريض 8 ٪ و 11 ٪ و 13 ٪ إضافية من سكان العالم لندرة المياه الجديدة أو المتفاقمة، على التوالي، بثقة >50 ٪ (في حين أن 1.3 مليار شخص يعيشون بالفعل في مناطق شحيحة المياه). وفي الوقت نفسه، ستحدث تحولات كبيرة في الموائل في المناطق الجغرافية الحيوية التي تحتوي على 1 ٪ (في المناطق المتأثرة عند 2 درجة مئوية) و 10 ٪ (3.5 درجة مئوية) و 74 ٪ (5 درجات مئوية) من أنواع النباتات الوعائية المتوطنة الحالية، على التوالي. تشير النتائج إلى نمو غير خطي للتأثيرات جنبًا إلى جنب مع ΔTg وتسلط الضوء على التفاوتات الإقليمية في أحجام التأثير ومستويات ΔTg الحرجة.
CGIAR CGSpace (Consu... arrow_drop_down CGIAR CGSpace (Consultative Group on International Agricultural Research)Article . 2014License: CC BYFull-Text: https://hdl.handle.net/10568/34462Data sources: Bielefeld Academic Search Engine (BASE)Publikationenserver der Georg-August-Universität GöttingenArticle . 2013 . Peer-reviewedLicense: CC BYGöttingen Research Online PublicationsArticle . 2017License: CC BYData sources: Göttingen Research Online PublicationsPublikationsserver der Humboldt-Universität zu BerlinArticle . 2013 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu BerlinUniversity of East Anglia: UEA Digital RepositoryArticle . 2013Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 58 citations 58 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!
visibility 83visibility views 83 download downloads 52 Powered bymore_vert CGIAR CGSpace (Consu... arrow_drop_down CGIAR CGSpace (Consultative Group on International Agricultural Research)Article . 2014License: CC BYFull-Text: https://hdl.handle.net/10568/34462Data sources: Bielefeld Academic Search Engine (BASE)Publikationenserver der Georg-August-Universität GöttingenArticle . 2013 . Peer-reviewedLicense: CC BYGöttingen Research Online PublicationsArticle . 2017License: CC BYData sources: Göttingen Research Online PublicationsPublikationsserver der Humboldt-Universität zu BerlinArticle . 2013 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu BerlinUniversity of East Anglia: UEA Digital RepositoryArticle . 2013Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type , Journal , Research 2013 Germany, France, United Kingdom, FrancePublisher:IOP Publishing Funded by:EC | ERMITAGEEC| ERMITAGEGerten, Dieter; Lucht, Wolfgang; Ostberg, Sebastian; Heinke, Jens; Kowarsch, Martin; Kreft, Holger; Kundzewicz, Zbigniew W.; Rastgooy, Johann; Warren, Rachel; Schellnhuber, Hans Joachim; Gerten, Dieter;; Lucht, Wolfgang;; Ostberg, Sebastian;; Heinke, Jens;; Kowarsch, Martin;; Kreft, Holger;; Kundzewicz, Zbigniew W;; Rastgooy, Johann;; Warren, Rachel;; Schellnhuber, Hans Joachim;;handle: 10568/34462
Cette étude de modélisation démontre à quel niveau d'élévation de la température moyenne mondiale (ΔTg) les régions seront exposées à des diminutions significatives de la disponibilité en eau douce et à des changements dans les écosystèmes terrestres. Les projections sont basées sur un nouvel ensemble cohérent de 152 scénarios climatiques (huit trajectoires ΔTg atteignant 1,5-5 ° C au-dessus des niveaux préindustriels d'ici 2100, chacune mise à l'échelle avec des schémas spatiaux de 19 modèles de circulation générale). Les résultats suggèrent que déjà à un ΔTg de 2 ° C et principalement dans les régions subtropicales, une pénurie d'eau plus élevée se produirait dans plus de 50% des 19 scénarios climatiques. D'importants changements biogéochimiques et structurels de la végétation se produiraient également à 2 ° C, mais principalement dans les écosystèmes subpolaires et semi-arides. D'autres régions seraient affectées à des niveaux de ΔTg plus élevés, avec une intensité plus faible ou avec une confiance plus faible. Au total, des niveaux moyens de réchauffement planétaire de 2 ° C, 3,5 ° C et 5 ° C sont simulés pour exposer 8%, 11% et 13% supplémentaires de la population mondiale à une pénurie d'eau nouvelle ou aggravée, respectivement, avec une confiance >50% (alors qu'environ1,3 milliard de personnes vivent déjà dans des régions pauvres en eau). Parallèlement, des transformations substantielles de l'habitat se produiraient dans les régions biogéographiques qui contiennent 1% (dans les zones touchées à 2 ° C), 10% (3,5 ° C) et 74% (5 ° C) des espèces de plantes vasculaires actuelles pondérées par l'endémisme, respectivement. Les résultats suggèrent une croissance non linéaire des impacts avec ΔTg et mettent en évidence les disparités régionales dans les amplitudes d'impact et les niveaux critiques de ΔTg. Este estudio de modelado demuestra a qué nivel de aumento de la temperatura media global (ΔTg) las regiones estarán expuestas a disminuciones significativas de la disponibilidad de agua dulce y cambios en los ecosistemas terrestres. Las proyecciones se basan en un nuevo conjunto consistente de 152 escenarios climáticos (ocho trayectorias de ΔTg que alcanzan 1.5–5 ° C por encima de los niveles preindustriales para 2100, cada una escalada con patrones espaciales de 19 modelos de circulación general). Los resultados sugieren que ya a una ΔTg de 2°C y principalmente en los subtrópicos, se produciría una mayor escasez de agua en >50% de los 19 escenarios climáticos. También se producirían cambios estructurales sustanciales biogeoquímicos y de vegetación a 2 ° C, pero principalmente en ecosistemas subpolares y semiáridos. Otras regiones se verían afectadas a niveles más altos de ΔTg, con menor intensidad o con menor confianza. En total, se simulan niveles medios de calentamiento global de 2 ° C, 3,5 ° C y 5 ° C para exponer a un 8%, 11% y 13% adicionales de la población mundial a una escasez de agua nueva o agravada, respectivamente, con >50% de confianza (mientras que ~1.300 millones de personas ya viven en regiones con escasez de agua). Al mismo tiempo, se producirían transformaciones sustanciales del hábitat en regiones biogeográficas que contienen el 1% (en zonas afectadas a 2 ° C), el 10% (3.5 ° C) y el 74% (5 ° C) de las especies de plantas vasculares ponderadas por endemismo actuales, respectivamente. Los resultados sugieren un crecimiento no lineal de los impactos junto con ΔTg y resaltan las disparidades regionales en las magnitudes de impacto y los niveles críticos de ΔTg. This modelling study demonstrates at what level of global mean temperature rise (ΔTg) regions will be exposed to significant decreases of freshwater availability and changes to terrestrial ecosystems. Projections are based on a new, consistent set of 152 climate scenarios (eight ΔTg trajectories reaching 1.5–5 ° C above pre-industrial levels by 2100, each scaled with spatial patterns from 19 general circulation models). The results suggest that already at a ΔTg of 2 ° C and mainly in the subtropics, higher water scarcity would occur in >50% out of the 19 climate scenarios. Substantial biogeochemical and vegetation structural changes would also occur at 2 ° C, but mainly in subpolar and semiarid ecosystems. Other regions would be affected at higher ΔTg levels, with lower intensity or with lower confidence. In total, mean global warming levels of 2 ° C, 3.5 ° C and 5 ° C are simulated to expose an additional 8%, 11% and 13% of the world population to new or aggravated water scarcity, respectively, with >50% confidence (while ∼1.3 billion people already live in water-scarce regions). Concurrently, substantial habitat transformations would occur in biogeographic regions that contain 1% (in zones affected at 2 ° C), 10% (3.5 ° C) and 74% (5 ° C) of present endemism-weighted vascular plant species, respectively. The results suggest nonlinear growth of impacts along with ΔTg and highlight regional disparities in impact magnitudes and critical ΔTg levels. توضح دراسة النمذجة هذه مستوى مناطق متوسط ارتفاع درجة الحرارة العالمية (ΔTg) التي ستتعرض لانخفاضات كبيرة في توافر المياه العذبة والتغيرات في النظم الإيكولوجية الأرضية. تستند التوقعات إلى مجموعة جديدة ومتسقة من 152 سيناريو مناخيًا (ثمانية مسارات ΔTg تصل إلى 1.5–5 درجة مئوية فوق مستويات ما قبل الصناعة بحلول عام 2100، تم قياس كل منها بأنماط مكانية من 19 نموذج دوران عام). تشير النتائج إلى أنه بالفعل عند درجة حرارة 2 درجة مئوية وبشكل أساسي في المناطق شبه الاستوائية، ستحدث ندرة مياه أعلى في أكثر من 50 ٪ من السيناريوهات المناخية التسعة عشر. كما ستحدث تغييرات هيكلية بيوكيميائية ونباتية كبيرة عند 2 درجة مئوية، ولكن بشكل أساسي في النظم الإيكولوجية تحت القطبية وشبه القاحلة. ستتأثر المناطق الأخرى عند مستويات ΔTg أعلى، بكثافة أقل أو بثقة أقل. في المجموع، تتم محاكاة متوسط مستويات الاحترار العالمي البالغة 2 درجة مئوية و 3.5 درجة مئوية و 5 درجات مئوية لتعريض 8 ٪ و 11 ٪ و 13 ٪ إضافية من سكان العالم لندرة المياه الجديدة أو المتفاقمة، على التوالي، بثقة >50 ٪ (في حين أن 1.3 مليار شخص يعيشون بالفعل في مناطق شحيحة المياه). وفي الوقت نفسه، ستحدث تحولات كبيرة في الموائل في المناطق الجغرافية الحيوية التي تحتوي على 1 ٪ (في المناطق المتأثرة عند 2 درجة مئوية) و 10 ٪ (3.5 درجة مئوية) و 74 ٪ (5 درجات مئوية) من أنواع النباتات الوعائية المتوطنة الحالية، على التوالي. تشير النتائج إلى نمو غير خطي للتأثيرات جنبًا إلى جنب مع ΔTg وتسلط الضوء على التفاوتات الإقليمية في أحجام التأثير ومستويات ΔTg الحرجة.
CGIAR CGSpace (Consu... arrow_drop_down CGIAR CGSpace (Consultative Group on International Agricultural Research)Article . 2014License: CC BYFull-Text: https://hdl.handle.net/10568/34462Data sources: Bielefeld Academic Search Engine (BASE)Publikationenserver der Georg-August-Universität GöttingenArticle . 2013 . Peer-reviewedLicense: CC BYGöttingen Research Online PublicationsArticle . 2017License: CC BYData sources: Göttingen Research Online PublicationsPublikationsserver der Humboldt-Universität zu BerlinArticle . 2013 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu BerlinUniversity of East Anglia: UEA Digital RepositoryArticle . 2013Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 58 citations 58 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!
visibility 83visibility views 83 download downloads 52 Powered bymore_vert CGIAR CGSpace (Consu... arrow_drop_down CGIAR CGSpace (Consultative Group on International Agricultural Research)Article . 2014License: CC BYFull-Text: https://hdl.handle.net/10568/34462Data sources: Bielefeld Academic Search Engine (BASE)Publikationenserver der Georg-August-Universität GöttingenArticle . 2013 . Peer-reviewedLicense: CC BYGöttingen Research Online PublicationsArticle . 2017License: CC BYData sources: Göttingen Research Online PublicationsPublikationsserver der Humboldt-Universität zu BerlinArticle . 2013 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu BerlinUniversity of East Anglia: UEA Digital RepositoryArticle . 2013Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type 2012Publisher:Copernicus GmbH Jens Heinke; Sebastian Ostberg; Sibyll Schaphoff; Katja Frieler; Christoph Müller; Dieter Gerten; Malte Meinshausen; Wolfgang Lucht;Abstract. In the ongoing political debate on climate change, global mean temperature change (ΔTglob) has become the yardstick by which mitigation costs, impacts from unavoided climate change, and adaptation requirements are discussed. For a scientifically informed discourse along these lines systematic assessments of climate change impacts as a function of ΔTglob are required. The current availability of climate change scenarios constrains this type of assessment to a narrow range of temperature change and/or a reduced ensemble of climate models. Here, a newly composed dataset of climate change scenarios is presented that addresses the specific requirements for global assessments of climate change impacts as a function of ΔTglob. A pattern-scaling approach is applied to extract generalized patterns of spatially explicit change in temperature, precipitation and cloudiness from 19 AOGCMs. The patterns are combined with scenarios of global mean temperature increase obtained from the reduced-complexity climate model MAGICC6 to create climate scenarios covering warming levels from 1.5 to 5 degrees above pre-industrial levels around the year 2100. The patterns are shown to sufficiently maintain the original AOGCMs' climate change properties, even though they, necessarily, utilize a simplified relationships between ΔTglob and changes in local climate properties. The dataset (made available online upon final publication of this paper) facilitates systematic analyses of climate change impacts as it covers a wider and finer-spaced range of climate change scenarios than the original AOGCM simulations.
https://doi.org/10.5... arrow_drop_down https://doi.org/10.5194/gmdd-5...Article . 2012 . Peer-reviewedLicense: CC BYData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/gmdd-5-3533-2012&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routeshybrid 8 citations 8 popularity Average influence Top 10% impulse Top 10% Powered by BIP!
more_vert https://doi.org/10.5... arrow_drop_down https://doi.org/10.5194/gmdd-5...Article . 2012 . Peer-reviewedLicense: CC BYData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/gmdd-5-3533-2012&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type 2012Publisher:Copernicus GmbH Jens Heinke; Sebastian Ostberg; Sibyll Schaphoff; Katja Frieler; Christoph Müller; Dieter Gerten; Malte Meinshausen; Wolfgang Lucht;Abstract. In the ongoing political debate on climate change, global mean temperature change (ΔTglob) has become the yardstick by which mitigation costs, impacts from unavoided climate change, and adaptation requirements are discussed. For a scientifically informed discourse along these lines systematic assessments of climate change impacts as a function of ΔTglob are required. The current availability of climate change scenarios constrains this type of assessment to a narrow range of temperature change and/or a reduced ensemble of climate models. Here, a newly composed dataset of climate change scenarios is presented that addresses the specific requirements for global assessments of climate change impacts as a function of ΔTglob. A pattern-scaling approach is applied to extract generalized patterns of spatially explicit change in temperature, precipitation and cloudiness from 19 AOGCMs. The patterns are combined with scenarios of global mean temperature increase obtained from the reduced-complexity climate model MAGICC6 to create climate scenarios covering warming levels from 1.5 to 5 degrees above pre-industrial levels around the year 2100. The patterns are shown to sufficiently maintain the original AOGCMs' climate change properties, even though they, necessarily, utilize a simplified relationships between ΔTglob and changes in local climate properties. The dataset (made available online upon final publication of this paper) facilitates systematic analyses of climate change impacts as it covers a wider and finer-spaced range of climate change scenarios than the original AOGCM simulations.
https://doi.org/10.5... arrow_drop_down https://doi.org/10.5194/gmdd-5...Article . 2012 . Peer-reviewedLicense: CC BYData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/gmdd-5-3533-2012&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routeshybrid 8 citations 8 popularity Average influence Top 10% impulse Top 10% Powered by BIP!
more_vert https://doi.org/10.5... arrow_drop_down https://doi.org/10.5194/gmdd-5...Article . 2012 . Peer-reviewedLicense: CC BYData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/gmdd-5-3533-2012&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Conference object , Journal 2018 Germany, France, France, France, FrancePublisher:IOP Publishing Funded by:NSF | Collaborative Research: E..., NSF | CNH: Pluvials, Droughts, ..., EC | HELIXNSF| Collaborative Research: EaSM2--Wildfires and Regional Climate Variability - Mechanisms, Modeling, and Prediction ,NSF| CNH: Pluvials, Droughts, Energetics, and the Mongol Empire ,EC| HELIXJia Yang; Kazuya Nishina; Richard Betts; Richard Betts; Sibyll Schaphoff; Louis François; Alexandra-Jane Henrot; Jinfeng Chang; Christopher P. O. Reyer; Catherine Morfopoulos; Katja Frieler; Philippe Ciais; Jörg Steinkamp; Rashid Rafique; Fang Zhao; Thomas Hickler; Hanqin Tian; Sebastian Ostberg; Anselmo García Cantú; Akihiko Ito; Shufen Pan;This paper evaluates the ability of eight global vegetation models to reproduce recent trends and inter-annual variability of biomass in natural terrestrial ecosystems. For the purpose of this evaluation, the simulated trajectories of biomass are expressed in terms of the relative rate of change in biomass (RRB), defined as the deviation of the actual rate of biomass turnover from its equilibrium counterpart. Cumulative changes in RRB explain long-term changes in biomass pools. RRB simulated by the global vegetation models is compared with its observational equivalent, derived from vegetation optical depth reconstructions of above-ground biomass (AGB) over the period 1993–2010. According to the RRB analysis, the rate of global biomass growth described by the ensemble of simulations substantially exceeds the observation. The observed fluctuations of global RRB are significantly correlated with El Niño Southern Oscillation events (ENSO), but only some of the simulations reproduce this correlation. However, the ENSO sensitivity of RRB in the tropics is not significant in the observation, while it is in some of the simulations. This mismatch points to an important limitation of the observed AGB reconstruction to capture biomass variations in tropical forests. Important discrepancies in RRB were also identified at the regional scale, in the tropical forests of Amazonia and Central Africa, as well as in the boreal forests of north-western America, western and central Siberia. In each of these regions, the RRBs derived from the simulations were analyzed in connection with underlying differences in net primary productivity and biomass turnover rate ̶as a basis for exploring in how far differences in simulated changes in biomass are attributed to the response of the carbon uptake to CO _2 increments, as well as to the model representation of factors affecting the rates of mortality and turnover of foliage and roots. Overall, our findings stress the usefulness of using RRB to evaluate complex vegetation models and highlight the importance of conducting further evaluations of both the actual rate of biomass turnover and its equilibrium counterpart, with special focus on their background values and sources of variation. In turn, this task would require the availability of more accurate multi-year observational data of biomass and net primary productivity for natural ecosystems, as well as detailed and updated information on land-cover classification.
Hyper Article en Lig... arrow_drop_down Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2018Full-Text: https://hal.science/hal-02903437Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2018Full-Text: https://hal.science/hal-02903437Data sources: Bielefeld Academic Search Engine (BASE)Fachrepositorium LebenswissenschaftenArticle . 2018License: CC BYData sources: Fachrepositorium Lebenswissenschaftenadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1088/1748-9326/aac63c&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 3 citations 3 popularity Average influence Average impulse Average Powered by BIP!
more_vert Hyper Article en Lig... arrow_drop_down Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2018Full-Text: https://hal.science/hal-02903437Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2018Full-Text: https://hal.science/hal-02903437Data sources: Bielefeld Academic Search Engine (BASE)Fachrepositorium LebenswissenschaftenArticle . 2018License: CC BYData sources: Fachrepositorium Lebenswissenschaftenadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1088/1748-9326/aac63c&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Conference object , Journal 2018 Germany, France, France, France, FrancePublisher:IOP Publishing Funded by:NSF | Collaborative Research: E..., NSF | CNH: Pluvials, Droughts, ..., EC | HELIXNSF| Collaborative Research: EaSM2--Wildfires and Regional Climate Variability - Mechanisms, Modeling, and Prediction ,NSF| CNH: Pluvials, Droughts, Energetics, and the Mongol Empire ,EC| HELIXJia Yang; Kazuya Nishina; Richard Betts; Richard Betts; Sibyll Schaphoff; Louis François; Alexandra-Jane Henrot; Jinfeng Chang; Christopher P. O. Reyer; Catherine Morfopoulos; Katja Frieler; Philippe Ciais; Jörg Steinkamp; Rashid Rafique; Fang Zhao; Thomas Hickler; Hanqin Tian; Sebastian Ostberg; Anselmo García Cantú; Akihiko Ito; Shufen Pan;This paper evaluates the ability of eight global vegetation models to reproduce recent trends and inter-annual variability of biomass in natural terrestrial ecosystems. For the purpose of this evaluation, the simulated trajectories of biomass are expressed in terms of the relative rate of change in biomass (RRB), defined as the deviation of the actual rate of biomass turnover from its equilibrium counterpart. Cumulative changes in RRB explain long-term changes in biomass pools. RRB simulated by the global vegetation models is compared with its observational equivalent, derived from vegetation optical depth reconstructions of above-ground biomass (AGB) over the period 1993–2010. According to the RRB analysis, the rate of global biomass growth described by the ensemble of simulations substantially exceeds the observation. The observed fluctuations of global RRB are significantly correlated with El Niño Southern Oscillation events (ENSO), but only some of the simulations reproduce this correlation. However, the ENSO sensitivity of RRB in the tropics is not significant in the observation, while it is in some of the simulations. This mismatch points to an important limitation of the observed AGB reconstruction to capture biomass variations in tropical forests. Important discrepancies in RRB were also identified at the regional scale, in the tropical forests of Amazonia and Central Africa, as well as in the boreal forests of north-western America, western and central Siberia. In each of these regions, the RRBs derived from the simulations were analyzed in connection with underlying differences in net primary productivity and biomass turnover rate ̶as a basis for exploring in how far differences in simulated changes in biomass are attributed to the response of the carbon uptake to CO _2 increments, as well as to the model representation of factors affecting the rates of mortality and turnover of foliage and roots. Overall, our findings stress the usefulness of using RRB to evaluate complex vegetation models and highlight the importance of conducting further evaluations of both the actual rate of biomass turnover and its equilibrium counterpart, with special focus on their background values and sources of variation. In turn, this task would require the availability of more accurate multi-year observational data of biomass and net primary productivity for natural ecosystems, as well as detailed and updated information on land-cover classification.
Hyper Article en Lig... arrow_drop_down Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2018Full-Text: https://hal.science/hal-02903437Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2018Full-Text: https://hal.science/hal-02903437Data sources: Bielefeld Academic Search Engine (BASE)Fachrepositorium LebenswissenschaftenArticle . 2018License: CC BYData sources: Fachrepositorium Lebenswissenschaftenadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1088/1748-9326/aac63c&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 3 citations 3 popularity Average influence Average impulse Average Powered by BIP!
more_vert Hyper Article en Lig... arrow_drop_down Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2018Full-Text: https://hal.science/hal-02903437Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2018Full-Text: https://hal.science/hal-02903437Data sources: Bielefeld Academic Search Engine (BASE)Fachrepositorium LebenswissenschaftenArticle . 2018License: CC BYData sources: Fachrepositorium Lebenswissenschaftenadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1088/1748-9326/aac63c&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Conference object , Other literature type , Journal 2019Embargo end date: 16 Mar 2019 Netherlands, France, United Kingdom, Germany, Switzerland, France, France, France, France, Japan, France, Netherlands, Netherlands, Canada, Spain, France, AustriaPublisher:Springer Science and Business Media LLC Funded by:EC | IMPACT2C, EC | HELIXEC| IMPACT2C ,EC| HELIXJeroen Steenbeek; Erwin Schmid; Tyler D. Eddy; Tyler D. Eddy; Tyler D. Eddy; Derek P. Tittensor; Derek P. Tittensor; Rene Orth; Rene Orth; Yadu Pokhrel; Joshua Elliott; Yusuke Satoh; Yusuke Satoh; Christian Folberth; Louis François; Andrew D. Friend; Catherine Morfopoulos; Nikolay Khabarov; Peter Lawrence; Naota Hanasaki; Michelle T. H. van Vliet; Akihiko Ito; Sonia I. Seneviratne; Veronika Huber; Thomas A. M. Pugh; Jinfeng Chang; Tobias Stacke; Philippe Ciais; Lila Warszawski; Jan Volkholz; Matthias Büchner; Yoshihide Wada; Christopher P. O. Reyer; Xuhui Wang; Xuhui Wang; Xuhui Wang; Dieter Gerten; Dieter Gerten; Sebastian Ostberg; Qiuhong Tang; Gen Sakurai; David A. Carozza; David A. Carozza; Christoph Müller; Jacob Schewe; Lutz Breuer; Delphine Deryng; Heike K. Lotze; Hannes Müller Schmied; Robert Vautard; Hyungjun Kim; Fang Zhao; Allard de Wit; Jörg Steinkamp; Katja Frieler; Simon N. Gosling; Lukas Gudmundsson; Marta Coll; Hanqin Tian;doi: 10.1038/s41467-019-08745-6 , 10.17863/cam.37807 , 10.60692/8dj48-81382 , 10.3929/ethz-b-000330244 , 10.60692/8mcvk-e7225
pmid: 30824763
pmc: PMC6397256
handle: 10261/181642
doi: 10.1038/s41467-019-08745-6 , 10.17863/cam.37807 , 10.60692/8dj48-81382 , 10.3929/ethz-b-000330244 , 10.60692/8mcvk-e7225
pmid: 30824763
pmc: PMC6397256
handle: 10261/181642
AbstractGlobal impact models represent process-level understanding of how natural and human systems may be affected by climate change. Their projections are used in integrated assessments of climate change. Here we test, for the first time, systematically across many important systems, how well such impact models capture the impacts of extreme climate conditions. Using the 2003 European heat wave and drought as a historical analogue for comparable events in the future, we find that a majority of models underestimate the extremeness of impacts in important sectors such as agriculture, terrestrial ecosystems, and heat-related human mortality, while impacts on water resources and hydropower are overestimated in some river basins; and the spread across models is often large. This has important implications for economic assessments of climate change impacts that rely on these models. It also means that societal risks from future extreme events may be greater than previously thought.
IIASA PURE arrow_drop_down Université Jean Monnet – Saint-Etienne: HALArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)École Polytechnique, Université Paris-Saclay: HALArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Memorial University of Newfoundland: Research RepositoryArticle . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Recolector de Ciencia Abierta, RECOLECTAArticle . 2019 . Peer-reviewedData sources: Recolector de Ciencia Abierta, RECOLECTAWageningen Staff PublicationsArticle . 2019License: CC BYData sources: Wageningen Staff PublicationsHochschulschriftenserver - Universität Frankfurt am MainArticle . 2019Data sources: Hochschulschriftenserver - Universität Frankfurt am MainPublication Server of Goethe University Frankfurt am MainArticle . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1038/s41467-019-08745-6&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen 202 citations 202 popularity Top 0.1% influence Top 10% impulse Top 0.1% Powered by BIP!
more_vert IIASA PURE arrow_drop_down Université Jean Monnet – Saint-Etienne: HALArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)École Polytechnique, Université Paris-Saclay: HALArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Memorial University of Newfoundland: Research RepositoryArticle . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Recolector de Ciencia Abierta, RECOLECTAArticle . 2019 . Peer-reviewedData sources: Recolector de Ciencia Abierta, RECOLECTAWageningen Staff PublicationsArticle . 2019License: CC BYData sources: Wageningen Staff PublicationsHochschulschriftenserver - Universität Frankfurt am MainArticle . 2019Data sources: Hochschulschriftenserver - Universität Frankfurt am MainPublication Server of Goethe University Frankfurt am MainArticle . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1038/s41467-019-08745-6&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Conference object , Other literature type , Journal 2019Embargo end date: 16 Mar 2019 Netherlands, France, United Kingdom, Germany, Switzerland, France, France, France, France, Japan, France, Netherlands, Netherlands, Canada, Spain, France, AustriaPublisher:Springer Science and Business Media LLC Funded by:EC | IMPACT2C, EC | HELIXEC| IMPACT2C ,EC| HELIXJeroen Steenbeek; Erwin Schmid; Tyler D. Eddy; Tyler D. Eddy; Tyler D. Eddy; Derek P. Tittensor; Derek P. Tittensor; Rene Orth; Rene Orth; Yadu Pokhrel; Joshua Elliott; Yusuke Satoh; Yusuke Satoh; Christian Folberth; Louis François; Andrew D. Friend; Catherine Morfopoulos; Nikolay Khabarov; Peter Lawrence; Naota Hanasaki; Michelle T. H. van Vliet; Akihiko Ito; Sonia I. Seneviratne; Veronika Huber; Thomas A. M. Pugh; Jinfeng Chang; Tobias Stacke; Philippe Ciais; Lila Warszawski; Jan Volkholz; Matthias Büchner; Yoshihide Wada; Christopher P. O. Reyer; Xuhui Wang; Xuhui Wang; Xuhui Wang; Dieter Gerten; Dieter Gerten; Sebastian Ostberg; Qiuhong Tang; Gen Sakurai; David A. Carozza; David A. Carozza; Christoph Müller; Jacob Schewe; Lutz Breuer; Delphine Deryng; Heike K. Lotze; Hannes Müller Schmied; Robert Vautard; Hyungjun Kim; Fang Zhao; Allard de Wit; Jörg Steinkamp; Katja Frieler; Simon N. Gosling; Lukas Gudmundsson; Marta Coll; Hanqin Tian;doi: 10.1038/s41467-019-08745-6 , 10.17863/cam.37807 , 10.60692/8dj48-81382 , 10.3929/ethz-b-000330244 , 10.60692/8mcvk-e7225
pmid: 30824763
pmc: PMC6397256
handle: 10261/181642
doi: 10.1038/s41467-019-08745-6 , 10.17863/cam.37807 , 10.60692/8dj48-81382 , 10.3929/ethz-b-000330244 , 10.60692/8mcvk-e7225
pmid: 30824763
pmc: PMC6397256
handle: 10261/181642
AbstractGlobal impact models represent process-level understanding of how natural and human systems may be affected by climate change. Their projections are used in integrated assessments of climate change. Here we test, for the first time, systematically across many important systems, how well such impact models capture the impacts of extreme climate conditions. Using the 2003 European heat wave and drought as a historical analogue for comparable events in the future, we find that a majority of models underestimate the extremeness of impacts in important sectors such as agriculture, terrestrial ecosystems, and heat-related human mortality, while impacts on water resources and hydropower are overestimated in some river basins; and the spread across models is often large. This has important implications for economic assessments of climate change impacts that rely on these models. It also means that societal risks from future extreme events may be greater than previously thought.
IIASA PURE arrow_drop_down Université Jean Monnet – Saint-Etienne: HALArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)École Polytechnique, Université Paris-Saclay: HALArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Memorial University of Newfoundland: Research RepositoryArticle . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Recolector de Ciencia Abierta, RECOLECTAArticle . 2019 . Peer-reviewedData sources: Recolector de Ciencia Abierta, RECOLECTAWageningen Staff PublicationsArticle . 2019License: CC BYData sources: Wageningen Staff PublicationsHochschulschriftenserver - Universität Frankfurt am MainArticle . 2019Data sources: Hochschulschriftenserver - Universität Frankfurt am MainPublication Server of Goethe University Frankfurt am MainArticle . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen 202 citations 202 popularity Top 0.1% influence Top 10% impulse Top 0.1% Powered by BIP!
more_vert IIASA PURE arrow_drop_down Université Jean Monnet – Saint-Etienne: HALArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)École Polytechnique, Université Paris-Saclay: HALArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Memorial University of Newfoundland: Research RepositoryArticle . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2019Full-Text: https://hal.science/hal-02895259Data sources: Bielefeld Academic Search Engine (BASE)Recolector de Ciencia Abierta, RECOLECTAArticle . 2019 . Peer-reviewedData sources: Recolector de Ciencia Abierta, RECOLECTAWageningen Staff PublicationsArticle . 2019License: CC BYData sources: Wageningen Staff PublicationsHochschulschriftenserver - Universität Frankfurt am MainArticle . 2019Data sources: Hochschulschriftenserver - Universität Frankfurt am MainPublication Server of Goethe University Frankfurt am MainArticle . 2019License: CC BYData sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1038/s41467-019-08745-6&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Journal 2013 Germany, France, United Kingdom, France, France, France, France, United KingdomPublisher:Proceedings of the National Academy of Sciences Funded by:EC | GREENCYCLESIIEC| GREENCYCLESIIAndrew D. Friend; F. Ian Woodward; Tim T. Rademacher; Ron Kahana; Sibyll Schaphoff; Richard Betts; Akihiko Ito; Andy Wiltshire; Rutger Dankers; Axel Kleidon; Pete Falloon; Wolfgang Lucht; Wolfgang Lucht; Philippe Ciais; Lila Warszawski; Nicolas Vuichard; Philippe Peylin; Patricia Cadule; Mark R. Lomas; Rozenn Keribin; Douglas B. Clark; Sebastian Ostberg; Kazuya Nishina; Ryan Pavlick;Future climate change and increasing atmospheric CO 2 are expected to cause major changes in vegetation structure and function over large fractions of the global land surface. Seven global vegetation models are used to analyze possible responses to future climate simulated by a range of general circulation models run under all four representative concentration pathway scenarios of changing concentrations of greenhouse gases. All 110 simulations predict an increase in global vegetation carbon to 2100, but with substantial variation between vegetation models. For example, at 4 °C of global land surface warming (510–758 ppm of CO 2 ), vegetation carbon increases by 52–477 Pg C (224 Pg C mean), mainly due to CO 2 fertilization of photosynthesis. Simulations agree on large regional increases across much of the boreal forest, western Amazonia, central Africa, western China, and southeast Asia, with reductions across southwestern North America, central South America, southern Mediterranean areas, southwestern Africa, and southwestern Australia. Four vegetation models display discontinuities across 4 °C of warming, indicating global thresholds in the balance of positive and negative influences on productivity and biomass. In contrast to previous global vegetation model studies, we emphasize the importance of uncertainties in projected changes in carbon residence times. We find, when all seven models are considered for one representative concentration pathway × general circulation model combination, such uncertainties explain 30% more variation in modeled vegetation carbon change than responses of net primary productivity alone, increasing to 151% for non-HYBRID4 models. A change in research priorities away from production and toward structural dynamics and demographic processes is recommended.
Proceedings of the N... arrow_drop_down Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2014Data sources: Bielefeld Academic Search Engine (BASE)Proceedings of the National Academy of SciencesArticle . 2013 . Peer-reviewedData sources: CrossrefÉcole Polytechnique, Université Paris-Saclay: HALArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Natural Environment Research Council: NERC Open Research ArchiveArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1073/pnas.1222477110&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen bronze 465 citations 465 popularity Top 0.1% influence Top 1% impulse Top 0.1% Powered by BIP!
more_vert Proceedings of the N... arrow_drop_down Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2014Data sources: Bielefeld Academic Search Engine (BASE)Proceedings of the National Academy of SciencesArticle . 2013 . Peer-reviewedData sources: CrossrefÉcole Polytechnique, Université Paris-Saclay: HALArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Natural Environment Research Council: NERC Open Research ArchiveArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1073/pnas.1222477110&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Journal 2013 Germany, France, United Kingdom, France, France, France, France, United KingdomPublisher:Proceedings of the National Academy of Sciences Funded by:EC | GREENCYCLESIIEC| GREENCYCLESIIAndrew D. Friend; F. Ian Woodward; Tim T. Rademacher; Ron Kahana; Sibyll Schaphoff; Richard Betts; Akihiko Ito; Andy Wiltshire; Rutger Dankers; Axel Kleidon; Pete Falloon; Wolfgang Lucht; Wolfgang Lucht; Philippe Ciais; Lila Warszawski; Nicolas Vuichard; Philippe Peylin; Patricia Cadule; Mark R. Lomas; Rozenn Keribin; Douglas B. Clark; Sebastian Ostberg; Kazuya Nishina; Ryan Pavlick;Future climate change and increasing atmospheric CO 2 are expected to cause major changes in vegetation structure and function over large fractions of the global land surface. Seven global vegetation models are used to analyze possible responses to future climate simulated by a range of general circulation models run under all four representative concentration pathway scenarios of changing concentrations of greenhouse gases. All 110 simulations predict an increase in global vegetation carbon to 2100, but with substantial variation between vegetation models. For example, at 4 °C of global land surface warming (510–758 ppm of CO 2 ), vegetation carbon increases by 52–477 Pg C (224 Pg C mean), mainly due to CO 2 fertilization of photosynthesis. Simulations agree on large regional increases across much of the boreal forest, western Amazonia, central Africa, western China, and southeast Asia, with reductions across southwestern North America, central South America, southern Mediterranean areas, southwestern Africa, and southwestern Australia. Four vegetation models display discontinuities across 4 °C of warming, indicating global thresholds in the balance of positive and negative influences on productivity and biomass. In contrast to previous global vegetation model studies, we emphasize the importance of uncertainties in projected changes in carbon residence times. We find, when all seven models are considered for one representative concentration pathway × general circulation model combination, such uncertainties explain 30% more variation in modeled vegetation carbon change than responses of net primary productivity alone, increasing to 151% for non-HYBRID4 models. A change in research priorities away from production and toward structural dynamics and demographic processes is recommended.
Proceedings of the N... arrow_drop_down Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2014Data sources: Bielefeld Academic Search Engine (BASE)Proceedings of the National Academy of SciencesArticle . 2013 . Peer-reviewedData sources: CrossrefÉcole Polytechnique, Université Paris-Saclay: HALArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Natural Environment Research Council: NERC Open Research ArchiveArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1073/pnas.1222477110&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen bronze 465 citations 465 popularity Top 0.1% influence Top 1% impulse Top 0.1% Powered by BIP!
more_vert Proceedings of the N... arrow_drop_down Publication Database PIK (Potsdam Institute for Climate Impact Research)Article . 2014Data sources: Bielefeld Academic Search Engine (BASE)Proceedings of the National Academy of SciencesArticle . 2013 . Peer-reviewedData sources: CrossrefÉcole Polytechnique, Université Paris-Saclay: HALArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Natural Environment Research Council: NERC Open Research ArchiveArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2014Data sources: Bielefeld Academic Search Engine (BASE)add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1073/pnas.1222477110&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Journal 2018Embargo end date: 01 Sep 2022 GermanyPublisher:IOP Publishing Sebastian Ostberg; Sebastian Ostberg; Petra Döll; Dieter Gerten; Dieter Gerten; Hannes Müller Schmied; Tim Trautmann; Fahad Saaed; Carl-Friedrich Schleussner; Carl-Friedrich Schleussner;To support implementation of the Paris Agreement, the new HAPPI ensemble of 20 bias-corrected simulations of four climate models was used to drive two global hydrological models, WaterGAP and LPJmL, for assessing freshwater-related hazards and risks in worlds approximately 1.5 °C and 2 °C warmer than pre-industrial. Quasi-stationary HAPPI simulations are better suited than transient CMIP-like simulations for assessing hazards at the two targeted long-term global warming (GW) levels. We analyzed seven hydrological hazard indicators that characterize freshwater-related hazards for humans, freshwater biota and vegetation. Using a strict definition for significant differences, we identified for all but one indicator that areas with either significantly wetter or drier conditions (calculated as percent changes from 2006–2015) are smaller in the 1.5 °C world. For example, 7 day high flow is projected to increase significantly on 11% and 21% of the global land area at 1.5 °C and 2 °C, respectively. However, differences between hydrological hazards at the two GW levels are significant on less than 12% of the area. GW affects a larger area and more people by increases—rather than by decreases—of mean annual and 1-in-10 dry year streamflow, 7 day high flow, and groundwater recharge. The opposite is true for 7 day low flow, maximum snow storage, and soil moisture in the driest month of the growing period. Mean annual streamflow shows the lowest projected percent changes of all indicators. Among country groups, low income countries and lower middle income countries are most affected by decreased low flows and increased high flows, respectively, while high income countries are least affected by such changes. The incremental impact between 1.5 °C and 2 °C on high flows would be felt most by low income and lower middle income countries, the effect on soil moisture and low flows most by high income countries.
Publication Database... arrow_drop_down Fachrepositorium LebenswissenschaftenArticle . 2018License: CC BYData sources: Fachrepositorium LebenswissenschaftenPublikationsserver der Humboldt-Universität zu BerlinArticle . 2018 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu Berlinadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1088/1748-9326/aab792&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 77 citations 77 popularity Top 1% influence Top 10% impulse Top 1% Powered by BIP!
visibility 64visibility views 64 download downloads 31 Powered bymore_vert Publication Database... arrow_drop_down Fachrepositorium LebenswissenschaftenArticle . 2018License: CC BYData sources: Fachrepositorium LebenswissenschaftenPublikationsserver der Humboldt-Universität zu BerlinArticle . 2018 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu Berlinadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1088/1748-9326/aab792&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Journal 2018Embargo end date: 01 Sep 2022 GermanyPublisher:IOP Publishing Sebastian Ostberg; Sebastian Ostberg; Petra Döll; Dieter Gerten; Dieter Gerten; Hannes Müller Schmied; Tim Trautmann; Fahad Saaed; Carl-Friedrich Schleussner; Carl-Friedrich Schleussner;To support implementation of the Paris Agreement, the new HAPPI ensemble of 20 bias-corrected simulations of four climate models was used to drive two global hydrological models, WaterGAP and LPJmL, for assessing freshwater-related hazards and risks in worlds approximately 1.5 °C and 2 °C warmer than pre-industrial. Quasi-stationary HAPPI simulations are better suited than transient CMIP-like simulations for assessing hazards at the two targeted long-term global warming (GW) levels. We analyzed seven hydrological hazard indicators that characterize freshwater-related hazards for humans, freshwater biota and vegetation. Using a strict definition for significant differences, we identified for all but one indicator that areas with either significantly wetter or drier conditions (calculated as percent changes from 2006–2015) are smaller in the 1.5 °C world. For example, 7 day high flow is projected to increase significantly on 11% and 21% of the global land area at 1.5 °C and 2 °C, respectively. However, differences between hydrological hazards at the two GW levels are significant on less than 12% of the area. GW affects a larger area and more people by increases—rather than by decreases—of mean annual and 1-in-10 dry year streamflow, 7 day high flow, and groundwater recharge. The opposite is true for 7 day low flow, maximum snow storage, and soil moisture in the driest month of the growing period. Mean annual streamflow shows the lowest projected percent changes of all indicators. Among country groups, low income countries and lower middle income countries are most affected by decreased low flows and increased high flows, respectively, while high income countries are least affected by such changes. The incremental impact between 1.5 °C and 2 °C on high flows would be felt most by low income and lower middle income countries, the effect on soil moisture and low flows most by high income countries.
Publication Database... arrow_drop_down Fachrepositorium LebenswissenschaftenArticle . 2018License: CC BYData sources: Fachrepositorium LebenswissenschaftenPublikationsserver der Humboldt-Universität zu BerlinArticle . 2018 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu Berlinadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1088/1748-9326/aab792&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 77 citations 77 popularity Top 1% influence Top 10% impulse Top 1% Powered by BIP!
visibility 64visibility views 64 download downloads 31 Powered bymore_vert Publication Database... arrow_drop_down Fachrepositorium LebenswissenschaftenArticle . 2018License: CC BYData sources: Fachrepositorium LebenswissenschaftenPublikationsserver der Humboldt-Universität zu BerlinArticle . 2018 . Peer-reviewedData sources: Publikationsserver der Humboldt-Universität zu Berlinadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1088/1748-9326/aab792&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu