Arctic sea-ice data, link to netCDF files

One of the clearest manifestations of ongoing global climate change is the dramatic retreat and thinning of the Arctic sea-ice cover. While all state-of-the-art climate models consistently reproduce the sign of these changes, they largely disagree on their magnitude, the reasons for which remain con...

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Main Author: Massonnet, François
Format: Dataset
Language:English
Published: PANGAEA 2018
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.889757
https://doi.org/10.1594/PANGAEA.889757
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spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.889757 2023-05-15T14:25:47+02:00 Arctic sea-ice data, link to netCDF files Massonnet, François 2018-05-09 application/zip, 231.9 MBytes https://doi.pangaea.de/10.1594/PANGAEA.889757 https://doi.org/10.1594/PANGAEA.889757 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.889757 https://doi.org/10.1594/PANGAEA.889757 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Massonnet, François; Vancoppenolle, Martin; Goosse, Hugues; Docquier, David; Fichefet, Thierry; Blanchard-Wrigglesworth, Edward (2018): Arctic sea-ice change tied to its mean state through thermodynamic processes. Nature Climate Change, 7 pp, https://doi.org/10.1038/s41558-018-0204-z Dataset 2018 ftpangaea https://doi.org/10.1594/PANGAEA.889757 https://doi.org/10.1038/s41558-018-0204-z 2023-01-20T09:11:00Z One of the clearest manifestations of ongoing global climate change is the dramatic retreat and thinning of the Arctic sea-ice cover. While all state-of-the-art climate models consistently reproduce the sign of these changes, they largely disagree on their magnitude, the reasons for which remain contentious. As such, consensual methods to reduce uncertainty in projections are lacking. Here, using the CMIP5 ensemble, we propose a process-oriented approach to revisit this issue. We show that inter-model differences in sea-ice loss and, more generally, in simulated sea-ice variability, can be traced to differences in the simulation of seasonal growth and melt. The way these processes are simulated is relatively independent of the complexity of the sea-ice model used, but rather a strong function of the background thickness. The larger role played by thermodynamic processes as sea ice thins further suggests the recent and projected reductions in sea-ice thickness induce a transition of the Arctic towards a state with enhanced volume seasonality but reduced interannual volume variability and persistence, before summer ice-free conditions eventually occur. These results prompt modelling groups to focus their priorities on the reduction of sea-ice thickness biases. Dataset Arctic Arctic Climate change Sea ice PANGAEA - Data Publisher for Earth & Environmental Science Arctic
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
description One of the clearest manifestations of ongoing global climate change is the dramatic retreat and thinning of the Arctic sea-ice cover. While all state-of-the-art climate models consistently reproduce the sign of these changes, they largely disagree on their magnitude, the reasons for which remain contentious. As such, consensual methods to reduce uncertainty in projections are lacking. Here, using the CMIP5 ensemble, we propose a process-oriented approach to revisit this issue. We show that inter-model differences in sea-ice loss and, more generally, in simulated sea-ice variability, can be traced to differences in the simulation of seasonal growth and melt. The way these processes are simulated is relatively independent of the complexity of the sea-ice model used, but rather a strong function of the background thickness. The larger role played by thermodynamic processes as sea ice thins further suggests the recent and projected reductions in sea-ice thickness induce a transition of the Arctic towards a state with enhanced volume seasonality but reduced interannual volume variability and persistence, before summer ice-free conditions eventually occur. These results prompt modelling groups to focus their priorities on the reduction of sea-ice thickness biases.
format Dataset
author Massonnet, François
spellingShingle Massonnet, François
Arctic sea-ice data, link to netCDF files
author_facet Massonnet, François
author_sort Massonnet, François
title Arctic sea-ice data, link to netCDF files
title_short Arctic sea-ice data, link to netCDF files
title_full Arctic sea-ice data, link to netCDF files
title_fullStr Arctic sea-ice data, link to netCDF files
title_full_unstemmed Arctic sea-ice data, link to netCDF files
title_sort arctic sea-ice data, link to netcdf files
publisher PANGAEA
publishDate 2018
url https://doi.pangaea.de/10.1594/PANGAEA.889757
https://doi.org/10.1594/PANGAEA.889757
geographic Arctic
geographic_facet Arctic
genre Arctic
Arctic
Climate change
Sea ice
genre_facet Arctic
Arctic
Climate change
Sea ice
op_source Supplement to: Massonnet, François; Vancoppenolle, Martin; Goosse, Hugues; Docquier, David; Fichefet, Thierry; Blanchard-Wrigglesworth, Edward (2018): Arctic sea-ice change tied to its mean state through thermodynamic processes. Nature Climate Change, 7 pp, https://doi.org/10.1038/s41558-018-0204-z
op_relation https://doi.pangaea.de/10.1594/PANGAEA.889757
https://doi.org/10.1594/PANGAEA.889757
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.889757
https://doi.org/10.1038/s41558-018-0204-z
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