neXtSIM: a new Lagrangian sea ice model
The Arctic sea ice cover has changed drastically over the last decades. Associated with these changes is a shift in dynamical regime seen by an increase of extreme fracturing events and an acceleration of sea ice drift. The highly non-linear dynamical response of sea ice to external forcing makes mo...
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2016
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ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00013353 2023-05-15T14:51:06+02:00 neXtSIM: a new Lagrangian sea ice model Rampal, Pierre Bouillon, Sylvain Ólason, Einar Morlighem, Mathieu 2016-05 electronic https://doi.org/10.5194/tc-10-1055-2016 https://noa.gwlb.de/receive/cop_mods_00013353 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00013309/tc-10-1055-2016.pdf https://tc.copernicus.org/articles/10/1055/2016/tc-10-1055-2016.pdf eng eng Copernicus Publications The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424 https://doi.org/10.5194/tc-10-1055-2016 https://noa.gwlb.de/receive/cop_mods_00013353 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00013309/tc-10-1055-2016.pdf https://tc.copernicus.org/articles/10/1055/2016/tc-10-1055-2016.pdf uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2016 ftnonlinearchiv https://doi.org/10.5194/tc-10-1055-2016 2022-02-08T22:55:39Z The Arctic sea ice cover has changed drastically over the last decades. Associated with these changes is a shift in dynamical regime seen by an increase of extreme fracturing events and an acceleration of sea ice drift. The highly non-linear dynamical response of sea ice to external forcing makes modelling these changes and the future evolution of Arctic sea ice a challenge for current models. It is, however, increasingly important that this challenge be better met, both because of the important role of sea ice in the climate system and because of the steady increase of industrial operations in the Arctic. In this paper we present a new dynamical/thermodynamical sea ice model called neXtSIM that is designed to address this challenge. neXtSIM is a continuous and fully Lagrangian model, whose momentum equation is discretised with the finite-element method. In this model, sea ice physics are driven by the combination of two core components: a model for sea ice dynamics built on a mechanical framework using an elasto-brittle rheology, and a model for sea ice thermodynamics providing damage healing for the mechanical framework. The evaluation of the model performance for the Arctic is presented for the period September 2007 to October 2008 and shows that observed multi-scale statistical properties of sea ice drift and deformation are well captured as well as the seasonal cycles of ice volume, area, and extent. These results show that neXtSIM is an appropriate tool for simulating sea ice over a wide range of spatial and temporal scales. Article in Journal/Newspaper Arctic Sea ice The Cryosphere Niedersächsisches Online-Archiv NOA Arctic The Cryosphere 10 3 1055 1073 |
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Niedersächsisches Online-Archiv NOA |
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English |
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article Verlagsveröffentlichung |
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article Verlagsveröffentlichung Rampal, Pierre Bouillon, Sylvain Ólason, Einar Morlighem, Mathieu neXtSIM: a new Lagrangian sea ice model |
topic_facet |
article Verlagsveröffentlichung |
description |
The Arctic sea ice cover has changed drastically over the last decades. Associated with these changes is a shift in dynamical regime seen by an increase of extreme fracturing events and an acceleration of sea ice drift. The highly non-linear dynamical response of sea ice to external forcing makes modelling these changes and the future evolution of Arctic sea ice a challenge for current models. It is, however, increasingly important that this challenge be better met, both because of the important role of sea ice in the climate system and because of the steady increase of industrial operations in the Arctic. In this paper we present a new dynamical/thermodynamical sea ice model called neXtSIM that is designed to address this challenge. neXtSIM is a continuous and fully Lagrangian model, whose momentum equation is discretised with the finite-element method. In this model, sea ice physics are driven by the combination of two core components: a model for sea ice dynamics built on a mechanical framework using an elasto-brittle rheology, and a model for sea ice thermodynamics providing damage healing for the mechanical framework. The evaluation of the model performance for the Arctic is presented for the period September 2007 to October 2008 and shows that observed multi-scale statistical properties of sea ice drift and deformation are well captured as well as the seasonal cycles of ice volume, area, and extent. These results show that neXtSIM is an appropriate tool for simulating sea ice over a wide range of spatial and temporal scales. |
format |
Article in Journal/Newspaper |
author |
Rampal, Pierre Bouillon, Sylvain Ólason, Einar Morlighem, Mathieu |
author_facet |
Rampal, Pierre Bouillon, Sylvain Ólason, Einar Morlighem, Mathieu |
author_sort |
Rampal, Pierre |
title |
neXtSIM: a new Lagrangian sea ice model |
title_short |
neXtSIM: a new Lagrangian sea ice model |
title_full |
neXtSIM: a new Lagrangian sea ice model |
title_fullStr |
neXtSIM: a new Lagrangian sea ice model |
title_full_unstemmed |
neXtSIM: a new Lagrangian sea ice model |
title_sort |
nextsim: a new lagrangian sea ice model |
publisher |
Copernicus Publications |
publishDate |
2016 |
url |
https://doi.org/10.5194/tc-10-1055-2016 https://noa.gwlb.de/receive/cop_mods_00013353 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00013309/tc-10-1055-2016.pdf https://tc.copernicus.org/articles/10/1055/2016/tc-10-1055-2016.pdf |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Sea ice The Cryosphere |
genre_facet |
Arctic Sea ice The Cryosphere |
op_relation |
The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424 https://doi.org/10.5194/tc-10-1055-2016 https://noa.gwlb.de/receive/cop_mods_00013353 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00013309/tc-10-1055-2016.pdf https://tc.copernicus.org/articles/10/1055/2016/tc-10-1055-2016.pdf |
op_rights |
uneingeschränkt info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5194/tc-10-1055-2016 |
container_title |
The Cryosphere |
container_volume |
10 |
container_issue |
3 |
container_start_page |
1055 |
op_container_end_page |
1073 |
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1766322166745268224 |