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  • Energy Research
  • 2025-2025
  • 6. Clean water
  • 15. Life on land
  • 16. Peace & justice

  • In the steppes of the Volga region on the southern chernozem in a long stationary experiment, the influence of weather conditions and mineral fertilizers on the yield of grain crops was revealed.It is shown how weather and climatic conditions affect plant productivity, responsiveness to fertilizers and their payback by crop.The features of climate change in the Volga steppe at the end of the 20th and beginning of the 21st centuries are considered.The parameters of changing the productivity of crops of a sixfield graincrop rotation for eight rotations associated with climate transformation are established.The obtained information serves as a database for building predictive mathematical models. В степи Поволжья на черноземе южном в длительном стационарном опыте выявлено влияние погодных условий и минеральных удобрений на урожайность зерновых культур. Показано, как погодные и климатические условия влияют на продуктивность растений, отзывчивость на удобрения и их окупаемость урожаем. Рассмотрены особенности изменения климата в степном Поволжье в конце 20гоначале 21 веков. Установлены параметры изменения продуктивности культур шестипольного зернопарового севооборота за восемь ротаций, связанные с трансформацией климата. Полученные сведения служат базой данных для построения прогнозных математических моделей.

    https://doi.org/10.2...arrow_drop_down
    https://doi.org/10.25680/vniia...
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      https://doi.org/10.25680/vniia...
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  • In the steppes of the Volga region on the southern chernozem in a long stationary experiment, the influence of weather conditions and mineral fertilizers on the yield of grain crops was revealed.It is shown how weather and climatic conditions affect plant productivity, responsiveness to fertilizers and their payback by crop.The features of climate change in the Volga steppe at the end of the 20th and beginning of the 21st centuries are considered.The parameters of changing the productivity of crops of a sixfield graincrop rotation for eight rotations associated with climate transformation are established.The obtained information serves as a database for building predictive mathematical models. В степи Поволжья на черноземе южном в длительном стационарном опыте выявлено влияние погодных условий и минеральных удобрений на урожайность зерновых культур. Показано, как погодные и климатические условия влияют на продуктивность растений, отзывчивость на удобрения и их окупаемость урожаем. Рассмотрены особенности изменения климата в степном Поволжье в конце 20гоначале 21 веков. Установлены параметры изменения продуктивности культур шестипольного зернопарового севооборота за восемь ротаций, связанные с трансформацией климата. Полученные сведения служат базой данных для построения прогнозных математических моделей.

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    Authors: orcid Nciizah, Adornis D;
    Nciizah, Adornis D
    ORCID
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    Nciizah, Adornis D in OpenAIRE
    Wakindiki, Isaiah IC;

    Predicted changes in rainfall intensity due to climate change are likely to influence key soil health parameters, especially structural attributes and crop growth. Variations in rainfall intensity will impact crop production negatively. It is therefore imperative to investigate the interaction between predicted increases in rainfall intensity and key soil health parameters, particularly in relation to soil structural attributes and plant growth. The objectives of this study were to determine the effects of rainfall intensity on soil crust formation and mode of seedling emergence in soils dominated by primary minerals. Soil samples were collected from the top 200 mm, air dried and then packed uniformly into plastic pots, which were perforated at the bottom. Three maize seeds of equal size were planted in a triangular pattern in each pot at a depth of 30 mm, after which the pots were pre-wetted by capillary. The samples were then subjected to simulated rainfall at 3 intensities, i.e., 30, 45 and 60 mm/h, for 5 min. Rainfall intensity significantly (P < 0.05) affected crust strength and mean emergence day (MED), but not emergence percentage (EMP) and shoot length (P > 0.05). The 60 mm/h rainfall intensity resulted in the highest crust strength and MED. The strength of crust for all three rainfall intensities was influenced by quartz content, soil organic matter, clay and hematite. Most seedlings emerged through cracks, which resulted in rainfall intensity having no significant effects on seedling EMP and shoot length. We concluded that any increase in rainfall intensity is likely to increase the severity of crusting in these soils. However, soils with extensive cracking are likely to have higher EMP and lower MED and more vigorous seedlings despite the strength of the crust. As a result, post-planting tillage methods that enhance crust cracking may be employed to enhance seedling emergence and growth in these soils.

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    Authors: orcid Nciizah, Adornis D;
    Nciizah, Adornis D
    ORCID
    Harvested from ORCID Public Data File

    Nciizah, Adornis D in OpenAIRE
    Wakindiki, Isaiah IC;

    Predicted changes in rainfall intensity due to climate change are likely to influence key soil health parameters, especially structural attributes and crop growth. Variations in rainfall intensity will impact crop production negatively. It is therefore imperative to investigate the interaction between predicted increases in rainfall intensity and key soil health parameters, particularly in relation to soil structural attributes and plant growth. The objectives of this study were to determine the effects of rainfall intensity on soil crust formation and mode of seedling emergence in soils dominated by primary minerals. Soil samples were collected from the top 200 mm, air dried and then packed uniformly into plastic pots, which were perforated at the bottom. Three maize seeds of equal size were planted in a triangular pattern in each pot at a depth of 30 mm, after which the pots were pre-wetted by capillary. The samples were then subjected to simulated rainfall at 3 intensities, i.e., 30, 45 and 60 mm/h, for 5 min. Rainfall intensity significantly (P < 0.05) affected crust strength and mean emergence day (MED), but not emergence percentage (EMP) and shoot length (P > 0.05). The 60 mm/h rainfall intensity resulted in the highest crust strength and MED. The strength of crust for all three rainfall intensities was influenced by quartz content, soil organic matter, clay and hematite. Most seedlings emerged through cracks, which resulted in rainfall intensity having no significant effects on seedling EMP and shoot length. We concluded that any increase in rainfall intensity is likely to increase the severity of crusting in these soils. However, soils with extensive cracking are likely to have higher EMP and lower MED and more vigorous seedlings despite the strength of the crust. As a result, post-planting tillage methods that enhance crust cracking may be employed to enhance seedling emergence and growth in these soils.

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    Authors: Open Data Nova Scotia;

    Temperature data from the Centre for Marine Applied Research's (CMAR) Coastal Monitoring Program. The original dataset includes data measured on intervals of 1 minute to 1 hour. The figure shows the daily average values for the waterbody, station, depth, time period, and quality control flags selected from the dropdown filters. The filtered dataset can be exported using the "Export" button on the right. To see other variables that were measured in this county, explore the original dataset (https://data.novascotia.ca/d/wpsu-7fer). To learn more about CMAR's Coastal Monitoring Program, visit https://cmar.ca/coastal-monitoring-program/

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    Authors: Open Data Nova Scotia;

    Temperature data from the Centre for Marine Applied Research's (CMAR) Coastal Monitoring Program. The original dataset includes data measured on intervals of 1 minute to 1 hour. The figure shows the daily average values for the waterbody, station, depth, time period, and quality control flags selected from the dropdown filters. The filtered dataset can be exported using the "Export" button on the right. To see other variables that were measured in this county, explore the original dataset (https://data.novascotia.ca/d/wpsu-7fer). To learn more about CMAR's Coastal Monitoring Program, visit https://cmar.ca/coastal-monitoring-program/

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    This repository contains VBA and ArcObjects code used to analyze plant distributions in digitized quadrats near Flagstaff Arizona, over the years 2002 - 2024. This code was used to produce the data presented in the Data Paper "Cover and density of southwestern ponderosa pine understory plants in permanent chart quadrats (2002-2024)" (Moore et al. 2025). There are 262 VBA functions used in this project, distributed over 13 modules and comprising 25,566 lines of code. The primary analytical master function is "RunAsBatch" in the module "H_WB_Analysis". This function runs several other functions that do the various steps of the analysis. In particular: The function "OrganizeData" in module "H_WB_Analysis" assembles all original datasets into a single workspace with a common naming convention, and adds verbatim fields to keep track of edits made to data. The function "ReviseShapefiles" in module "H_WB_Analysis" corrects species misspellings and misidentifications. The function "ConvertPointShapefiles" in module "H_WB_Analysis" converts point features to small polygons, deletes a few extraneous objects, adds a few observations that were missed in the digitizing, switches species designations from Cover to Density or vice-versa if necessary, and rotates quadrats if they were mapped with the wrong orientation. The function "AddEmptyFeaturesAndFeatureClasses" in module "H_WB_Analysis" adds empty feature classes if a survey was done on that quadrat in that year but no features were found. These empty feature classes distinguish these cases from times when no survey was conducted. The function "RepairOverlappingPolygons" in the module "More_Margaret_Functions" fixes cases when polygons for a single observation are digitized twice, or when separate polygons for a single species overlap. The function "RecreateSubsetsOfConvertedDatasets" in the module "More_Margaret_Functions" combines all newly-corrected feature classes into a new workspace, and creates two global feature classes containing all cover and all density observations. The function "AddEmptyFeaturesAndFeatureClassesToCleaned" in module "H_WB_Analysis" adds empty feature classes to the newly corrected feature classes if a survey was done on that quadrat in that year but no features were found. These empty feature classes distinguish these cases from times when no survey was conducted. The function "ShiftFinishedShapefilesToCoordinateSystem" in module "H_WB_Analysis" correctly georeferences all feature classes and saves to a new workspace. Prior to this step all plant locations were in a local 1-square-meter coordinate system based on the 1-square-meter quadrat. The function "ExportFinalDataset" in module "H_WB_Analysis" removes extraneous and verbatim fields, and exports the final version of the dataset to a new workspace. The function "SummarizeSpeciesBySite" in module "More_Margaret_Functions" analyzes all the feature classes to determine which species were observed at each site. The function "SummarizeSpeciesByCorrectQuadrat" in module "More_Margaret_Functions" analyzes all the feature classes to determine which species were observed at each quadrat. The function "SummarizeYearByCorrectQuadratByYear" in module "More_Margaret_Functions" analyzes all the feature classes to determine which quadrats were surveyed each year. The function "ExportSubsetsOfSpeciesShapefiles" in module "Margaret_Functions_3" extracts each species individually from the full dataset, and saves them in a series of nested folders suitable for Integral Projection Model functions in R. The function "CreateFinalTables" in module "H_WB_Analysis" produces the final summary tables intended for distribution with the data, including a list of plant species observed, a summary of the basal area per species by quadrat and year, summary data describing all quadrats and overstory plots, and tabular versions of the global cover and density feature classes. The primary map export function is "ExportImages" in the module "Margaret", and is run separately from the 14 functions run in the batch file above. This map-making function creates common plant species symbology that can be applied to all 1,877 maps, and exports individual maps for each quadrat and for each year. This function is best run from an ArcMap document with no data in it, which is why it is run separately from the other functions. Note: These functions are written in ArcObjects and VBA, and therefore can only be run in ArcMap. ArcGIS Pro cannot run them. Moore, M. M., J. S. Jenness, D. C. Laughlin, R. T. Strahan, J. D. Bakker, H. E. Dowling, and J. D. Springer. 2022. Cover and density of southwestern ponderosa pine understory plants in permanent chart quadrats (2002-2020). Ecology 103(5): e3661. https://doi.org/10.1002/ ecy.3661 Moore, M. M., Jenness, J. S, Laughlin, D. C., Strahan, R. T., Bakker, J. D., Dowling, H. E., and Springer, J. D. 2025. Cover and density of southwestern ponderosa pine understory plants in permanent chart quadrats (2002-2020+). Fort Collins, CO: Forest Service Research Data Archive. Updated February 2025.

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    This repository contains VBA and ArcObjects code used to analyze plant distributions in digitized quadrats near Flagstaff Arizona, over the years 2002 - 2024. This code was used to produce the data presented in the Data Paper "Cover and density of southwestern ponderosa pine understory plants in permanent chart quadrats (2002-2024)" (Moore et al. 2025). There are 262 VBA functions used in this project, distributed over 13 modules and comprising 25,566 lines of code. The primary analytical master function is "RunAsBatch" in the module "H_WB_Analysis". This function runs several other functions that do the various steps of the analysis. In particular: The function "OrganizeData" in module "H_WB_Analysis" assembles all original datasets into a single workspace with a common naming convention, and adds verbatim fields to keep track of edits made to data. The function "ReviseShapefiles" in module "H_WB_Analysis" corrects species misspellings and misidentifications. The function "ConvertPointShapefiles" in module "H_WB_Analysis" converts point features to small polygons, deletes a few extraneous objects, adds a few observations that were missed in the digitizing, switches species designations from Cover to Density or vice-versa if necessary, and rotates quadrats if they were mapped with the wrong orientation. The function "AddEmptyFeaturesAndFeatureClasses" in module "H_WB_Analysis" adds empty feature classes if a survey was done on that quadrat in that year but no features were found. These empty feature classes distinguish these cases from times when no survey was conducted. The function "RepairOverlappingPolygons" in the module "More_Margaret_Functions" fixes cases when polygons for a single observation are digitized twice, or when separate polygons for a single species overlap. The function "RecreateSubsetsOfConvertedDatasets" in the module "More_Margaret_Functions" combines all newly-corrected feature classes into a new workspace, and creates two global feature classes containing all cover and all density observations. The function "AddEmptyFeaturesAndFeatureClassesToCleaned" in module "H_WB_Analysis" adds empty feature classes to the newly corrected feature classes if a survey was done on that quadrat in that year but no features were found. These empty feature classes distinguish these cases from times when no survey was conducted. The function "ShiftFinishedShapefilesToCoordinateSystem" in module "H_WB_Analysis" correctly georeferences all feature classes and saves to a new workspace. Prior to this step all plant locations were in a local 1-square-meter coordinate system based on the 1-square-meter quadrat. The function "ExportFinalDataset" in module "H_WB_Analysis" removes extraneous and verbatim fields, and exports the final version of the dataset to a new workspace. The function "SummarizeSpeciesBySite" in module "More_Margaret_Functions" analyzes all the feature classes to determine which species were observed at each site. The function "SummarizeSpeciesByCorrectQuadrat" in module "More_Margaret_Functions" analyzes all the feature classes to determine which species were observed at each quadrat. The function "SummarizeYearByCorrectQuadratByYear" in module "More_Margaret_Functions" analyzes all the feature classes to determine which quadrats were surveyed each year. The function "ExportSubsetsOfSpeciesShapefiles" in module "Margaret_Functions_3" extracts each species individually from the full dataset, and saves them in a series of nested folders suitable for Integral Projection Model functions in R. The function "CreateFinalTables" in module "H_WB_Analysis" produces the final summary tables intended for distribution with the data, including a list of plant species observed, a summary of the basal area per species by quadrat and year, summary data describing all quadrats and overstory plots, and tabular versions of the global cover and density feature classes. The primary map export function is "ExportImages" in the module "Margaret", and is run separately from the 14 functions run in the batch file above. This map-making function creates common plant species symbology that can be applied to all 1,877 maps, and exports individual maps for each quadrat and for each year. This function is best run from an ArcMap document with no data in it, which is why it is run separately from the other functions. Note: These functions are written in ArcObjects and VBA, and therefore can only be run in ArcMap. ArcGIS Pro cannot run them. Moore, M. M., J. S. Jenness, D. C. Laughlin, R. T. Strahan, J. D. Bakker, H. E. Dowling, and J. D. Springer. 2022. Cover and density of southwestern ponderosa pine understory plants in permanent chart quadrats (2002-2020). Ecology 103(5): e3661. https://doi.org/10.1002/ ecy.3661 Moore, M. M., Jenness, J. S, Laughlin, D. C., Strahan, R. T., Bakker, J. D., Dowling, H. E., and Springer, J. D. 2025. Cover and density of southwestern ponderosa pine understory plants in permanent chart quadrats (2002-2020+). Fort Collins, CO: Forest Service Research Data Archive. Updated February 2025.

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  • Authors: Hörsch, Jonas; Hofmann, Fabian; Schlachtberger, David; Glaum, Philipp; +5 Authors

    PyPSA-Eur is an open model dataset of the European power system at the transmission network level that covers the full ENTSO-E area. It can be built using the code provided at https://github.com/PyPSA/PyPSA-eur. It contains alternating current lines at and above 220 kV voltage level and all high voltage direct current lines, substations, an open database of conventional power plants, time series for electrical demand and variable renewable generator availability, and geographic potentials for the expansion of wind and solar power. Not all data dependencies are shipped with the code repository, since git is not suited for handling large changing files. Instead we provide separate data bundles to be downloaded and extracted as noted in the documentation. This is the full data bundle to be used for rigorous research. It includes large bathymetry and natural protection area datasets. While the code in PyPSA-Eur is released as free software under the MIT, different licenses and terms of use apply to the various input data, which are summarised below: corine/* CORINE Land Cover (CLC) database Source: https://land.copernicus.eu/pan-european/corine-land-cover/clc-2012/ Terms of Use: https://land.copernicus.eu/pan-european/corine-land-cover/clc-2012?tab=metadata natura/* Natura 2000 natural protection areas Source: https://www.eea.europa.eu/data-and-maps/data/natura-10 Terms of Use: https://www.eea.europa.eu/data-and-maps/data/natura-10#tab-metadata gebco/GEBCO_2014_2D.nc GEBCO bathymetric dataset Source: https://www.gebco.net/data_and_products/gridded_bathymetry_data/version_20141103/ Terms of Use: https://www.gebco.net/data_and_products/gridded_bathymetry_data/documents/gebco_2014_historic.pdf je-e-21.03.02.xls Population and GDP data for Swiss Cantons Source: https://www.bfs.admin.ch/bfs/en/home/news/whats-new.assetdetail.7786557.html Terms of Use: https://www.bfs.admin.ch/bfs/en/home/fso/swiss-federal-statistical-office/terms-of-use.html https://www.bfs.admin.ch/bfs/de/home/bfs/oeffentliche-statistik/copyright.html nama_10r_3popgdp.tsv.gz Population by NUTS3 region Source: http://appsso.eurostat.ec.europa.eu/nui/show.do?dataset=nama_10r_3popgdp&lang=en Terms of Use: https://ec.europa.eu/eurostat/about/policies/copyright GDP_per_capita_PPP_1990_2015_v2.nc Gross Domestic Product per capita (PPP) from years 1999 to 2015 Rectangular cutout for European countries in PyPSA-Eur, including a 10 km buffer Kummu et al. "Data from: Gridded global datasets for Gross Domestic Product and Human Development Index over 1990-2015" Source: https://doi.org/10.1038/sdata.2018.4 and associated dataset https://doi.org/10.1038/sdata.2018.4 ppp_2019_1km_Aggregated.tif The spatial distribution of population in 2020: Estimated total number of people per grid-cell. The dataset is available to download in Geotiff format at a resolution of 30 arc (approximately 1km at the equator). The projection is Geographic Coordinate System, WGS84. The units are number of people per pixel. The mapping approach is Random Forest-based dasymetric redistribution. Rectangular cutout for non-NUTS3 countries in PyPSA-Eur, i.e. MD and UA, including a 10 km buffer WorldPop (www.worldpop.org - School of Geography and Environmental Science, University of Southampton; Department of Geography and Geosciences, University of Louisville; Departement de Geographie, Universite de Namur) and Center for International Earth Science Information Network (CIESIN), Columbia University (2018). Global High Resolution Population Denominators Project - Funded by The Bill and Melinda Gates Foundation (OPP1134076). https://dx.doi.org/10.5258/SOTON/WP00647 Source: https://data.humdata.org/dataset/worldpop-population-counts-for-world and https://hub.worldpop.org/geodata/summary?id=24777 License: Creative Commons Attribution 4.0 International Licens data/bundle/era5-HDD-per-country.csv - Link: https://gist.github.com/fneum/d99e24e19da423038fd55fe3a4ddf875- License: CC-BY 4.0- Contains country-level heating degree days in Europe for 1941-2023. Used for rescaling heat demand in weather years not covered by energy balance statistics. data/bundle/era5-runoff-per-country.csv - Link: https://gist.github.com/fneum/d99e24e19da423038fd55fe3a4ddf875- License: CC-BY 4.0- Contains country-level daily sum of runoff in Europe for 1941-2023. Used for rescaling hydro-electricity availability in weather years not covered by EIA hydro-generation statistics. shipdensity_global.zip Global Shipping Traffic Density Creative Commons Attribution 4.0 https://datacatalog.worldbank.org/search/dataset/0037580/Global-Shipping-Traffic-Density seawater_temperature.nc Global Ocean Physics Reanalysis Link: https://data.marine.copernicus.eu/product/GLOBAL_MULTIYEAR_PHY_001_030/services License: https://marine.copernicus.eu/user-corner/service-commitments-and-licence

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  • Authors: Hörsch, Jonas; Hofmann, Fabian; Schlachtberger, David; Glaum, Philipp; +5 Authors

    PyPSA-Eur is an open model dataset of the European power system at the transmission network level that covers the full ENTSO-E area. It can be built using the code provided at https://github.com/PyPSA/PyPSA-eur. It contains alternating current lines at and above 220 kV voltage level and all high voltage direct current lines, substations, an open database of conventional power plants, time series for electrical demand and variable renewable generator availability, and geographic potentials for the expansion of wind and solar power. Not all data dependencies are shipped with the code repository, since git is not suited for handling large changing files. Instead we provide separate data bundles to be downloaded and extracted as noted in the documentation. This is the full data bundle to be used for rigorous research. It includes large bathymetry and natural protection area datasets. While the code in PyPSA-Eur is released as free software under the MIT, different licenses and terms of use apply to the various input data, which are summarised below: corine/* CORINE Land Cover (CLC) database Source: https://land.copernicus.eu/pan-european/corine-land-cover/clc-2012/ Terms of Use: https://land.copernicus.eu/pan-european/corine-land-cover/clc-2012?tab=metadata natura/* Natura 2000 natural protection areas Source: https://www.eea.europa.eu/data-and-maps/data/natura-10 Terms of Use: https://www.eea.europa.eu/data-and-maps/data/natura-10#tab-metadata gebco/GEBCO_2014_2D.nc GEBCO bathymetric dataset Source: https://www.gebco.net/data_and_products/gridded_bathymetry_data/version_20141103/ Terms of Use: https://www.gebco.net/data_and_products/gridded_bathymetry_data/documents/gebco_2014_historic.pdf je-e-21.03.02.xls Population and GDP data for Swiss Cantons Source: https://www.bfs.admin.ch/bfs/en/home/news/whats-new.assetdetail.7786557.html Terms of Use: https://www.bfs.admin.ch/bfs/en/home/fso/swiss-federal-statistical-office/terms-of-use.html https://www.bfs.admin.ch/bfs/de/home/bfs/oeffentliche-statistik/copyright.html nama_10r_3popgdp.tsv.gz Population by NUTS3 region Source: http://appsso.eurostat.ec.europa.eu/nui/show.do?dataset=nama_10r_3popgdp&lang=en Terms of Use: https://ec.europa.eu/eurostat/about/policies/copyright GDP_per_capita_PPP_1990_2015_v2.nc Gross Domestic Product per capita (PPP) from years 1999 to 2015 Rectangular cutout for European countries in PyPSA-Eur, including a 10 km buffer Kummu et al. "Data from: Gridded global datasets for Gross Domestic Product and Human Development Index over 1990-2015" Source: https://doi.org/10.1038/sdata.2018.4 and associated dataset https://doi.org/10.1038/sdata.2018.4 ppp_2019_1km_Aggregated.tif The spatial distribution of population in 2020: Estimated total number of people per grid-cell. The dataset is available to download in Geotiff format at a resolution of 30 arc (approximately 1km at the equator). The projection is Geographic Coordinate System, WGS84. The units are number of people per pixel. The mapping approach is Random Forest-based dasymetric redistribution. Rectangular cutout for non-NUTS3 countries in PyPSA-Eur, i.e. MD and UA, including a 10 km buffer WorldPop (www.worldpop.org - School of Geography and Environmental Science, University of Southampton; Department of Geography and Geosciences, University of Louisville; Departement de Geographie, Universite de Namur) and Center for International Earth Science Information Network (CIESIN), Columbia University (2018). Global High Resolution Population Denominators Project - Funded by The Bill and Melinda Gates Foundation (OPP1134076). https://dx.doi.org/10.5258/SOTON/WP00647 Source: https://data.humdata.org/dataset/worldpop-population-counts-for-world and https://hub.worldpop.org/geodata/summary?id=24777 License: Creative Commons Attribution 4.0 International Licens data/bundle/era5-HDD-per-country.csv - Link: https://gist.github.com/fneum/d99e24e19da423038fd55fe3a4ddf875- License: CC-BY 4.0- Contains country-level heating degree days in Europe for 1941-2023. Used for rescaling heat demand in weather years not covered by energy balance statistics. data/bundle/era5-runoff-per-country.csv - Link: https://gist.github.com/fneum/d99e24e19da423038fd55fe3a4ddf875- License: CC-BY 4.0- Contains country-level daily sum of runoff in Europe for 1941-2023. Used for rescaling hydro-electricity availability in weather years not covered by EIA hydro-generation statistics. shipdensity_global.zip Global Shipping Traffic Density Creative Commons Attribution 4.0 https://datacatalog.worldbank.org/search/dataset/0037580/Global-Shipping-Traffic-Density seawater_temperature.nc Global Ocean Physics Reanalysis Link: https://data.marine.copernicus.eu/product/GLOBAL_MULTIYEAR_PHY_001_030/services License: https://marine.copernicus.eu/user-corner/service-commitments-and-licence

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    Authors: ESHYA MUJAHID MUKHTAR; HANID MUKHTAR;

    Agricultural production depends upon certain crucial inputs e.g., water, fertilizer etc. In the less developed regions of South Asia in general, and the indo-Pakistan sub-continent in particular, the use of these inputs depends not only upon the financial affordability but also upon the institutional accessibility of farmers to these inputs. Besides high economic costs, bureaucratic controls and corruption regarding the distribution of inputs have created problems of limited accessibility, especially to the small farmers. In the absence of any credit, information and/or input distribution networks, the use of these inputs, and related productivity gains, become confined to that class of farmers which not only has better access to these inputs but is capable of using them in the best possible way e.g. use of water and fertilizer in the appropriate amount and at the appropriate time. This paper attempts to study how input use and input productivity vary across farm sizes, with some reference to the infrastructural and institutional factors, whose development play an important role in improving the distribution and productivity of inputs. For such an analysis, a comparison of the two Punjabs i.e. Pakistani and Indian Punjabs, presents an ideal framework, Separated by a national boundary since 1947, the two Punjabs enjoy a common history and culture, similar agricultural practices and agro-climatic conditions, Government policies in the two Punjabs, however, have not only differed between the two provinces at the same time, but also over time in the same province. It may be noted that due to certain policy measures, land distribution, tenancy conditions, promotion of agricultural co-operatives and provision of infrastructural features, such as roads and electricity, are relatively more improved in Indian than Pakistani Punjab.

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    The Pakistan Development Review
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    Authors: ESHYA MUJAHID MUKHTAR; HANID MUKHTAR;

    Agricultural production depends upon certain crucial inputs e.g., water, fertilizer etc. In the less developed regions of South Asia in general, and the indo-Pakistan sub-continent in particular, the use of these inputs depends not only upon the financial affordability but also upon the institutional accessibility of farmers to these inputs. Besides high economic costs, bureaucratic controls and corruption regarding the distribution of inputs have created problems of limited accessibility, especially to the small farmers. In the absence of any credit, information and/or input distribution networks, the use of these inputs, and related productivity gains, become confined to that class of farmers which not only has better access to these inputs but is capable of using them in the best possible way e.g. use of water and fertilizer in the appropriate amount and at the appropriate time. This paper attempts to study how input use and input productivity vary across farm sizes, with some reference to the infrastructural and institutional factors, whose development play an important role in improving the distribution and productivity of inputs. For such an analysis, a comparison of the two Punjabs i.e. Pakistani and Indian Punjabs, presents an ideal framework, Separated by a national boundary since 1947, the two Punjabs enjoy a common history and culture, similar agricultural practices and agro-climatic conditions, Government policies in the two Punjabs, however, have not only differed between the two provinces at the same time, but also over time in the same province. It may be noted that due to certain policy measures, land distribution, tenancy conditions, promotion of agricultural co-operatives and provision of infrastructural features, such as roads and electricity, are relatively more improved in Indian than Pakistani Punjab.

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    The Pakistan Development Review
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    Authors: orcid bw Larmola, Tuula;
    Larmola, Tuula
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    Andersson, Erik; orcid bw Balkovic, Juraj;
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    +15 Authors

    The global goal to mitigate climate change (CC) is to achieve net zero greenhouse gas emissions (GHGE) by 2050; the European Union (EU) aim is to cut GHGE at least by 55% already by 2030. These ambition targets require new GHGE mitigation measures across all land use sectors (LULUCF), where wetlands, as carbon (C) rich ecosystem, can effectively contribute to climate targets, biodiversity, and water-related ecosystem services. Natural peatlands accumulate C effectively due to water-logged conditions. However, they can turn into high GHG sources if they are drained, therefore there is still need to enhance knowledge regarding how and/or how much C is sequestered or released by peatlands after their restoration, as well as the socioeconomic effects.&#8220;ALFAwetlands - Restoration for the future&#8221; (www.alfawetlands.eu) is a Horizon Europe funded project (2022-2026), which is coordinated by Luke and carried out at local to EU levels with 15 partners across Europe. It&#8217;s main goal, in short, is to mitigate CC while supporting biodiversity and ecosystem services (BES) and being socially just and rewarding. This includes, e.g., increasing the knowledge about C storage and release in peatlands, specifically after restoration. While, in terms of C fluxes, focussing on peatlands, the project scope is larger and includes additionally floodplains, coastal wetlands and few artificial wetlands. ALFAwetlands will develop and indicate management alternatives for wetlands including such that have been or will be restored during this project. Measures under this project are not restricted to ecological restoration but include rehabilitation and re-vegetation action to improve ecosystem conditions (e.g., peatland forest: continuous-cover-forestry, cultivated peatlands: paludiculture). Studies are conducted in 9 Living Labs (LL&#8217;s) including 30 sites, which are located in wetlands in different parts of Europe (north-south gradient). At the local level, LL&#8217;s support and integrate interdisciplinary and multi-actor research on ecological, environmental, economic, and social issues. Experimental data from local sites are scaled-up and will be utilized e.g., by models to gain and understanding the potential impacts of upscaled wetland restoration measures. To achieve ALFAwetlands goals, 5 research workpackages are being implemented, namely: 1)improve geospatial knowledge base of wetlands, 2)co-create socially fair and rewarding pathways for wetland restoration, 3)estimate effects of restoration on GHGE and BES, with the data achieved from field experiments, 4)develop policy relevant scenarios for CC and BES, and 5)study societal impacts of wetland restoration. The project will also encourage stakeholders to utilise outputs and support their active participation in wetland management.

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    Authors: orcid bw Larmola, Tuula;
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    Andersson, Erik; orcid bw Balkovic, Juraj;
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    +15 Authors

    The global goal to mitigate climate change (CC) is to achieve net zero greenhouse gas emissions (GHGE) by 2050; the European Union (EU) aim is to cut GHGE at least by 55% already by 2030. These ambition targets require new GHGE mitigation measures across all land use sectors (LULUCF), where wetlands, as carbon (C) rich ecosystem, can effectively contribute to climate targets, biodiversity, and water-related ecosystem services. Natural peatlands accumulate C effectively due to water-logged conditions. However, they can turn into high GHG sources if they are drained, therefore there is still need to enhance knowledge regarding how and/or how much C is sequestered or released by peatlands after their restoration, as well as the socioeconomic effects.&#8220;ALFAwetlands - Restoration for the future&#8221; (www.alfawetlands.eu) is a Horizon Europe funded project (2022-2026), which is coordinated by Luke and carried out at local to EU levels with 15 partners across Europe. It&#8217;s main goal, in short, is to mitigate CC while supporting biodiversity and ecosystem services (BES) and being socially just and rewarding. This includes, e.g., increasing the knowledge about C storage and release in peatlands, specifically after restoration. While, in terms of C fluxes, focussing on peatlands, the project scope is larger and includes additionally floodplains, coastal wetlands and few artificial wetlands. ALFAwetlands will develop and indicate management alternatives for wetlands including such that have been or will be restored during this project. Measures under this project are not restricted to ecological restoration but include rehabilitation and re-vegetation action to improve ecosystem conditions (e.g., peatland forest: continuous-cover-forestry, cultivated peatlands: paludiculture). Studies are conducted in 9 Living Labs (LL&#8217;s) including 30 sites, which are located in wetlands in different parts of Europe (north-south gradient). At the local level, LL&#8217;s support and integrate interdisciplinary and multi-actor research on ecological, environmental, economic, and social issues. Experimental data from local sites are scaled-up and will be utilized e.g., by models to gain and understanding the potential impacts of upscaled wetland restoration measures. To achieve ALFAwetlands goals, 5 research workpackages are being implemented, namely: 1)improve geospatial knowledge base of wetlands, 2)co-create socially fair and rewarding pathways for wetland restoration, 3)estimate effects of restoration on GHGE and BES, with the data achieved from field experiments, 4)develop policy relevant scenarios for CC and BES, and 5)study societal impacts of wetland restoration. The project will also encourage stakeholders to utilise outputs and support their active participation in wetland management.

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  • image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Authors: orcid Cuartas, J;
    Cuartas, J
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    Bhatia, A; Carter, D; Cluver, L; +9 Authors

    The climate crisis is the biggest threat to the health, development, and wellbeing of the current and future generations. While there is extensive evidence on the direct impacts of climate change on human livelihood, there is little evidence on how children and young people are affected, and even less discussion and evidence on how the climate crisis could affect violence against children.In this commentary, we review selected research to assess the links between the climate crisis and violence against children.We employ a social-ecological perspective as an overarching framework to organize findings from the literature and call attention to increased violence against children as a specific, yet under-examined, direct and indirect consequence of the climate crisis.Using such a perspective, we examine how the climate crisis exacerbates the risk of violence against children at the continually intersecting and interacting levels of society, community, family, and the individual levels. We propose increased risk of armed conflict, forced displacement, poverty, income inequality, disruptions in critical health and social services, and mental health problems as key mechanisms linking the climate crisis and heightened risk of violence against children. Furthermore, we posit that the climate crisis serves as a threat multiplier, compounding existing vulnerabilities and inequities within populations and having harsher consequences in settings, communities, households, and for children already experiencing adversities.We conclude with a call for urgent efforts from researchers, practitioners, and policymakers to further investigate the specific empirical links between the climate crisis and violence against children and to design, test, implement, fund, and scale evidence-based, rights-based, and child friendly prevention, support, and response strategies to address violence against children.

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    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Child Abuse & Neglect
    Article . 2025 . Peer-reviewed
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      Child Abuse & Neglect
      Article . 2025 . Peer-reviewed
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  • image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Authors: orcid Cuartas, J;
    Cuartas, J
    ORCID
    Harvested from ORCID Public Data File

    Cuartas, J in OpenAIRE
    Bhatia, A; Carter, D; Cluver, L; +9 Authors

    The climate crisis is the biggest threat to the health, development, and wellbeing of the current and future generations. While there is extensive evidence on the direct impacts of climate change on human livelihood, there is little evidence on how children and young people are affected, and even less discussion and evidence on how the climate crisis could affect violence against children.In this commentary, we review selected research to assess the links between the climate crisis and violence against children.We employ a social-ecological perspective as an overarching framework to organize findings from the literature and call attention to increased violence against children as a specific, yet under-examined, direct and indirect consequence of the climate crisis.Using such a perspective, we examine how the climate crisis exacerbates the risk of violence against children at the continually intersecting and interacting levels of society, community, family, and the individual levels. We propose increased risk of armed conflict, forced displacement, poverty, income inequality, disruptions in critical health and social services, and mental health problems as key mechanisms linking the climate crisis and heightened risk of violence against children. Furthermore, we posit that the climate crisis serves as a threat multiplier, compounding existing vulnerabilities and inequities within populations and having harsher consequences in settings, communities, households, and for children already experiencing adversities.We conclude with a call for urgent efforts from researchers, practitioners, and policymakers to further investigate the specific empirical links between the climate crisis and violence against children and to design, test, implement, fund, and scale evidence-based, rights-based, and child friendly prevention, support, and response strategies to address violence against children.

    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Oxford University Re...arrow_drop_down
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    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Child Abuse & Neglect
    Article . 2025 . Peer-reviewed
    License: Elsevier TDM
    Data sources: Crossref
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      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Oxford University Re...arrow_drop_down
      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
      Child Abuse & Neglect
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    Authors: Open Data Nova Scotia;

    Temperature data from the Centre for Marine Applied Research's (CMAR) Coastal Monitoring Program. The original dataset includes data measured on intervals of 1 minute to 1 hour. The figure shows the daily average values for the waterbody, station, depth, time period, and quality control flags selected from the dropdown filters. The filtered dataset can be exported using the "Export" button on the right. To see other variables that were measured in this county, explore the original dataset (https://data.novascotia.ca/d/x9dy-aai9). To learn more about CMAR's Coastal Monitoring Program, visit https://cmar.ca/coastal-monitoring-program/.

    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ Lunarisarrow_drop_down
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    Lunaris
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      Lunaris
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    Authors: Open Data Nova Scotia;

    Temperature data from the Centre for Marine Applied Research's (CMAR) Coastal Monitoring Program. The original dataset includes data measured on intervals of 1 minute to 1 hour. The figure shows the daily average values for the waterbody, station, depth, time period, and quality control flags selected from the dropdown filters. The filtered dataset can be exported using the "Export" button on the right. To see other variables that were measured in this county, explore the original dataset (https://data.novascotia.ca/d/x9dy-aai9). To learn more about CMAR's Coastal Monitoring Program, visit https://cmar.ca/coastal-monitoring-program/.

    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ Lunarisarrow_drop_down
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    Lunaris
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  • Authors: orcid Farooq, Umar;
    Farooq, Umar
    ORCID
    Harvested from ORCID Public Data File

    Farooq, Umar in OpenAIRE

    Global lakes hold about 87% of the freshwater. However, climate change has posed a severe threat to these freshwater resources. Evaporation (E) is a major water loss from lakes, and the strong coupling between lake E and changes in atmospheric conditions in a warming climate leads to temporal and spatial variability in water loss through E, making it challenging for water resource management. This dissertation examines such spatiotemporal variability in global lake E in response to climate change, investigates its environmental controls, and identifies regions with large sensitivities to climate changes. Using a state-of-science Lake, Ice, Snow, and Sediment Simulator (LISSS) that is a lake model within the Community Land Model (CLM), it is shown that the large spatial variability of global lake E is modulated by the vapor pressure difference (e_D) between lake surface and overlying air. The e_D also causes higher nighttime lake E, which contributes more to the spatial variability of global lake E than daytime lake E. The performance of the Penman method (PM) is also evaluated against observations and the LISSS modeling results in estimating global lake E. It is shown that the PM overestimates lake E due to a strong bias in the net radiation (Rn) and lake water heat storage (G). Using the LISSS simulated Rn and G in the PM, however, the PM performance is largely improved and the PM E becomes comparable to the LISSS E. The global lake E trend over 1951 - 1978 is analyzed, which shows a decreasing E trend. Such a declined global lake E was largely caused by the decreased downward shortwave solar radiation. The global lake E was switched from the decreased trend over 1951-1978 to an increased trend over 1981-2016 with an accelerated trend of 0.76 mm yr-1. The tropical, arid, and temperate climate regions lakes contribute 66% to the increasing trend despite covering only 38% of the global lake surface area. Such a change in the global lake E trend was attributed to the increased vapor pressure deficit in a warmer climate. The model projection indicates that the mean global lake E will increase by 13% by the end of the 21st century under the Representative Concentration Pathway (RCP) 8.5 emissions scenario, relative to the 1985-2000 mean global lake E. The changes in lake E are expected to be more pronounced in North America, equatorial South America, Africa, northern Europe, Siberia, and Southeast Asia due to increased interannual variability. The results in this dissertation indicate that the widespread but heterogeneous increase in the global lake E threatens the crucial socioeconomic benefits that lakes provide to human society.

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  • Authors: orcid Farooq, Umar;
    Farooq, Umar
    ORCID
    Harvested from ORCID Public Data File

    Farooq, Umar in OpenAIRE

    Global lakes hold about 87% of the freshwater. However, climate change has posed a severe threat to these freshwater resources. Evaporation (E) is a major water loss from lakes, and the strong coupling between lake E and changes in atmospheric conditions in a warming climate leads to temporal and spatial variability in water loss through E, making it challenging for water resource management. This dissertation examines such spatiotemporal variability in global lake E in response to climate change, investigates its environmental controls, and identifies regions with large sensitivities to climate changes. Using a state-of-science Lake, Ice, Snow, and Sediment Simulator (LISSS) that is a lake model within the Community Land Model (CLM), it is shown that the large spatial variability of global lake E is modulated by the vapor pressure difference (e_D) between lake surface and overlying air. The e_D also causes higher nighttime lake E, which contributes more to the spatial variability of global lake E than daytime lake E. The performance of the Penman method (PM) is also evaluated against observations and the LISSS modeling results in estimating global lake E. It is shown that the PM overestimates lake E due to a strong bias in the net radiation (Rn) and lake water heat storage (G). Using the LISSS simulated Rn and G in the PM, however, the PM performance is largely improved and the PM E becomes comparable to the LISSS E. The global lake E trend over 1951 - 1978 is analyzed, which shows a decreasing E trend. Such a declined global lake E was largely caused by the decreased downward shortwave solar radiation. The global lake E was switched from the decreased trend over 1951-1978 to an increased trend over 1981-2016 with an accelerated trend of 0.76 mm yr-1. The tropical, arid, and temperate climate regions lakes contribute 66% to the increasing trend despite covering only 38% of the global lake surface area. Such a change in the global lake E trend was attributed to the increased vapor pressure deficit in a warmer climate. The model projection indicates that the mean global lake E will increase by 13% by the end of the 21st century under the Representative Concentration Pathway (RCP) 8.5 emissions scenario, relative to the 1985-2000 mean global lake E. The changes in lake E are expected to be more pronounced in North America, equatorial South America, Africa, northern Europe, Siberia, and Southeast Asia due to increased interannual variability. The results in this dissertation indicate that the widespread but heterogeneous increase in the global lake E threatens the crucial socioeconomic benefits that lakes provide to human society.

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