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description Publicationkeyboard_double_arrow_right Article , Journal 2019 France, Australia, Norway, Australia, NorwayPublisher:Springer Science and Business Media LLC Funded by:EC | ICE-ARC, DFG | ArctiC Amplification: Cli..., RCN | Ice-algal and under-ice p... +2 projectsEC| ICE-ARC ,DFG| ArctiC Amplification: Climate Relevant Atmospheric and SurfaCe Processes, and Feedback Mechanisms (AC)3 ,RCN| Ice-algal and under-ice phytoplankton bloom dynamics in a changing Arctic icescape. ,RCN| Oil spill and newly formed sea ice detection, characterization, and mapping in the Barents Sea using remote sensing by SAR ,RCN| Centre for Integrated Remote Sensing and Forecasting for Arctic Operations (CIRFA)Sebastian Gerland; Robert M. Graham; Arild Sundfjord; Von P. Walden; Christine Provost; Glen E. Liston; Achim Randelhoff; Bin Cheng; Jari Haapala; Ilker Fer; Nathalie Sennéchael; Agneta Fransson; Dmitry Divine; Ioanna Merkouriadi; Annette Rinke; Algot Kristoffer Peterson; Algot Kristoffer Peterson; Mats A. Granskog; Lars Henrik Smedsrud; Lars Henrik Smedsrud; Philipp Assmy; Stephen R. Hudson; J. King; Polona Itkin; Lana Cohen; Malin Johansson; Amelie Meyer; Amelie Meyer; Harald Steen; Pedro Duarte; Anja Rösel; Gunnar Spreen;AbstractA large retreat of sea-ice in the ‘stormy’ Atlantic Sector of the Arctic Ocean has become evident through a series of record minima for the winter maximum sea-ice extent since 2015. Results from the Norwegian young sea ICE (N-ICE2015) expedition, a five-month-long (Jan-Jun) drifting ice station in first and second year pack-ice north of Svalbard, showcase how sea-ice in this region is frequently affected by passing winter storms. Here we synthesise the interdisciplinary N-ICE2015 dataset, including independent observations of the atmosphere, snow, sea-ice, ocean, and ecosystem. We build upon recent results and illustrate the different mechanisms through which winter storms impact the coupled Arctic sea-ice system. These short-lived and episodic synoptic-scale events transport pulses of heat and moisture into the Arctic, which temporarily reduce radiative cooling and henceforth ice growth. Cumulative snowfall from each sequential storm deepens the snow pack and insulates the sea-ice, further inhibiting ice growth throughout the remaining winter season. Strong winds fracture the ice cover, enhance ocean-ice-atmosphere heat fluxes, and make the ice more susceptible to lateral melt. In conclusion, the legacy of Arctic winter storms for sea-ice and the ice-associated ecosystem in the Atlantic Sector lasts far beyond their short lifespan.
Hyper Article en Lig... arrow_drop_down University of Bergen: Bergen Open Research Archive (BORA-UiB)Article . 2019License: CC BYFull-Text: https://hdl.handle.net/1956/20663Data sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2019Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2019Data sources: Bielefeld Academic Search Engine (BASE)École Polytechnique, Université Paris-Saclay: HALArticle . 2019Data sources: Bielefeld Academic Search Engine (BASE)Munin - Open Research ArchiveArticle . 2019 . Peer-reviewedData sources: Munin - Open Research ArchiveBergen Open Research Archive - UiBArticle . 2019 . Peer-reviewedLicense: CC BYData sources: Bergen Open Research Archive - UiBUniversity of Tasmania: UTas ePrintsArticle . 2019Data 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/s41598-019-45574-5&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 67 citations 67 popularity Top 1% influence Top 10% impulse Top 1% 
Powered by BIP!more_vert Hyper Article en Lig... arrow_drop_down University of Bergen: Bergen Open Research Archive (BORA-UiB)Article . 2019License: CC BYFull-Text: https://hdl.handle.net/1956/20663Data sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2019Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2019Data sources: Bielefeld Academic Search Engine (BASE)École Polytechnique, Université Paris-Saclay: HALArticle . 2019Data sources: Bielefeld Academic Search Engine (BASE)Munin - Open Research ArchiveArticle . 2019 . Peer-reviewedData sources: Munin - Open Research ArchiveBergen Open Research Archive - UiBArticle . 2019 . Peer-reviewedLicense: CC BYData sources: Bergen Open Research Archive - UiBUniversity of Tasmania: UTas ePrintsArticle . 2019Data 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/s41598-019-45574-5&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.eu
description Publicationkeyboard_double_arrow_right Article , Journal 2019 France, Australia, Norway, Australia, NorwayPublisher:Springer Science and Business Media LLC Funded by:EC | ICE-ARC, DFG | ArctiC Amplification: Cli..., RCN | Ice-algal and under-ice p... +2 projectsEC| ICE-ARC ,DFG| ArctiC Amplification: Climate Relevant Atmospheric and SurfaCe Processes, and Feedback Mechanisms (AC)3 ,RCN| Ice-algal and under-ice phytoplankton bloom dynamics in a changing Arctic icescape. ,RCN| Oil spill and newly formed sea ice detection, characterization, and mapping in the Barents Sea using remote sensing by SAR ,RCN| Centre for Integrated Remote Sensing and Forecasting for Arctic Operations (CIRFA)Sebastian Gerland; Robert M. Graham; Arild Sundfjord; Von P. Walden; Christine Provost; Glen E. Liston; Achim Randelhoff; Bin Cheng; Jari Haapala; Ilker Fer; Nathalie Sennéchael; Agneta Fransson; Dmitry Divine; Ioanna Merkouriadi; Annette Rinke; Algot Kristoffer Peterson; Algot Kristoffer Peterson; Mats A. Granskog; Lars Henrik Smedsrud; Lars Henrik Smedsrud; Philipp Assmy; Stephen R. Hudson; J. King; Polona Itkin; Lana Cohen; Malin Johansson; Amelie Meyer; Amelie Meyer; Harald Steen; Pedro Duarte; Anja Rösel; Gunnar Spreen;AbstractA large retreat of sea-ice in the ‘stormy’ Atlantic Sector of the Arctic Ocean has become evident through a series of record minima for the winter maximum sea-ice extent since 2015. Results from the Norwegian young sea ICE (N-ICE2015) expedition, a five-month-long (Jan-Jun) drifting ice station in first and second year pack-ice north of Svalbard, showcase how sea-ice in this region is frequently affected by passing winter storms. Here we synthesise the interdisciplinary N-ICE2015 dataset, including independent observations of the atmosphere, snow, sea-ice, ocean, and ecosystem. We build upon recent results and illustrate the different mechanisms through which winter storms impact the coupled Arctic sea-ice system. These short-lived and episodic synoptic-scale events transport pulses of heat and moisture into the Arctic, which temporarily reduce radiative cooling and henceforth ice growth. Cumulative snowfall from each sequential storm deepens the snow pack and insulates the sea-ice, further inhibiting ice growth throughout the remaining winter season. Strong winds fracture the ice cover, enhance ocean-ice-atmosphere heat fluxes, and make the ice more susceptible to lateral melt. In conclusion, the legacy of Arctic winter storms for sea-ice and the ice-associated ecosystem in the Atlantic Sector lasts far beyond their short lifespan.
Hyper Article en Lig... arrow_drop_down University of Bergen: Bergen Open Research Archive (BORA-UiB)Article . 2019License: CC BYFull-Text: https://hdl.handle.net/1956/20663Data sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2019Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2019Data sources: Bielefeld Academic Search Engine (BASE)École Polytechnique, Université Paris-Saclay: HALArticle . 2019Data sources: Bielefeld Academic Search Engine (BASE)Munin - Open Research ArchiveArticle . 2019 . Peer-reviewedData sources: Munin - Open Research ArchiveBergen Open Research Archive - UiBArticle . 2019 . Peer-reviewedLicense: CC BYData sources: Bergen Open Research Archive - UiBUniversity of Tasmania: UTas ePrintsArticle . 2019Data 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/s41598-019-45574-5&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 67 citations 67 popularity Top 1% influence Top 10% impulse Top 1% Powered by BIP!more_vert Hyper Article en Lig... arrow_drop_down University of Bergen: Bergen Open Research Archive (BORA-UiB)Article . 2019License: CC BYFull-Text: https://hdl.handle.net/1956/20663Data sources: Bielefeld Academic Search Engine (BASE)Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQArticle . 2019Data sources: Bielefeld Academic Search Engine (BASE)Institut national des sciences de l'Univers: HAL-INSUArticle . 2019Data sources: Bielefeld Academic Search Engine (BASE)École Polytechnique, Université Paris-Saclay: HALArticle . 2019Data sources: Bielefeld Academic Search Engine (BASE)Munin - Open Research ArchiveArticle . 2019 . Peer-reviewedData sources: Munin - Open Research ArchiveBergen Open Research Archive - UiBArticle . 2019 . Peer-reviewedLicense: CC BYData sources: Bergen Open Research Archive - UiBUniversity of Tasmania: UTas ePrintsArticle . 2019Data 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/s41598-019-45574-5&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.eu