Relationships between Arctic sea ice drift and strength modelled by NEMO-LIM3.6

Sea ice cover and thickness have substantially decreased in the Arctic Ocean since the beginning of the satellite era. As a result, sea ice strength has been reduced, allowing more deformation and fracturing and leading to increased sea ice drift speed. We use the version 3.6 of the global ocean–sea...

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Published in:Biogeosciences
Main Authors: Docquier, David, Massonnet, François, Barthélemy, Antoine, Tandon, Neil, Lecomte, Olivier, Fichefet, Thierry
Other Authors: UCL - SST/ELI/ELIC - Earth & Climate
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus GmbH 2017
Subjects:
Online Access:http://hdl.handle.net/2078.1/192309
https://doi.org/10.5194/tc-11-2829-2017
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spelling ftunistlouisbrus:oai:dial.uclouvain.be:boreal:192309 2023-05-15T14:54:51+02:00 Relationships between Arctic sea ice drift and strength modelled by NEMO-LIM3.6 Docquier, David Massonnet, François Barthélemy, Antoine Tandon, Neil Lecomte, Olivier Fichefet, Thierry UCL - SST/ELI/ELIC - Earth & Climate 2017 http://hdl.handle.net/2078.1/192309 https://doi.org/10.5194/tc-11-2829-2017 eng eng Copernicus GmbH boreal:192309 http://hdl.handle.net/2078.1/192309 doi:10.5194/tc-11-2829-2017 urn:ISSN:1994-0416 urn:EISSN:1994-0424 info:eu-repo/semantics/openAccess The Cryosphere, Vol. 11, p. 829-2846 info:eu-repo/semantics/article 2017 ftunistlouisbrus https://doi.org/10.5194/tc-11-2829-2017 2018-01-31T23:16:36Z Sea ice cover and thickness have substantially decreased in the Arctic Ocean since the beginning of the satellite era. As a result, sea ice strength has been reduced, allowing more deformation and fracturing and leading to increased sea ice drift speed. We use the version 3.6 of the global ocean–sea ice NEMO-LIM model (Nucleus for European Modelling of the Ocean coupled to the Louvain-laNeuve sea Ice Model), satellite, buoy and submarine observations, as well as reanalysis data over the period from 1979 to 2013 to study these relationships. Overall, the model agrees well with observations in terms of sea ice extent, concentration and thickness. The seasonal cycle of sea ice drift speed is reasonably well reproduced by the model. NEMOLIM3.6 is able to capture the relationships between the seasonal cycles of sea ice drift speed, concentration and thickness, with higher drift speed for both lower concentration and lower thickness, in agreement with observations. Model experiments are carried out to test the sensitivity of Arctic sea ice drift speed, thickness and concentration to changes in sea ice strength parameter P ∗ . These show that higher values of P ∗ generally lead to lower sea ice deformation and lower sea ice thickness, and that no single value of P ∗ is the best option for reproducing the observed drift speed and thickness. The methodology proposed in this analysis provides a benchmark for a further model intercomparison related to the relationships between sea ice drift speed and strength, which is especially relevant in the context of the upcoming Coupled Model Intercomparison Project 6 (CMIP6). Article in Journal/Newspaper Arctic Arctic Ocean Sea ice The Cryosphere DIAL@USL-B (Université Saint-Louis, Bruxelles) Arctic Arctic Ocean Biogeosciences 18 8 2649 2662
institution Open Polar
collection DIAL@USL-B (Université Saint-Louis, Bruxelles)
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language English
description Sea ice cover and thickness have substantially decreased in the Arctic Ocean since the beginning of the satellite era. As a result, sea ice strength has been reduced, allowing more deformation and fracturing and leading to increased sea ice drift speed. We use the version 3.6 of the global ocean–sea ice NEMO-LIM model (Nucleus for European Modelling of the Ocean coupled to the Louvain-laNeuve sea Ice Model), satellite, buoy and submarine observations, as well as reanalysis data over the period from 1979 to 2013 to study these relationships. Overall, the model agrees well with observations in terms of sea ice extent, concentration and thickness. The seasonal cycle of sea ice drift speed is reasonably well reproduced by the model. NEMOLIM3.6 is able to capture the relationships between the seasonal cycles of sea ice drift speed, concentration and thickness, with higher drift speed for both lower concentration and lower thickness, in agreement with observations. Model experiments are carried out to test the sensitivity of Arctic sea ice drift speed, thickness and concentration to changes in sea ice strength parameter P ∗ . These show that higher values of P ∗ generally lead to lower sea ice deformation and lower sea ice thickness, and that no single value of P ∗ is the best option for reproducing the observed drift speed and thickness. The methodology proposed in this analysis provides a benchmark for a further model intercomparison related to the relationships between sea ice drift speed and strength, which is especially relevant in the context of the upcoming Coupled Model Intercomparison Project 6 (CMIP6).
author2 UCL - SST/ELI/ELIC - Earth & Climate
format Article in Journal/Newspaper
author Docquier, David
Massonnet, François
Barthélemy, Antoine
Tandon, Neil
Lecomte, Olivier
Fichefet, Thierry
spellingShingle Docquier, David
Massonnet, François
Barthélemy, Antoine
Tandon, Neil
Lecomte, Olivier
Fichefet, Thierry
Relationships between Arctic sea ice drift and strength modelled by NEMO-LIM3.6
author_facet Docquier, David
Massonnet, François
Barthélemy, Antoine
Tandon, Neil
Lecomte, Olivier
Fichefet, Thierry
author_sort Docquier, David
title Relationships between Arctic sea ice drift and strength modelled by NEMO-LIM3.6
title_short Relationships between Arctic sea ice drift and strength modelled by NEMO-LIM3.6
title_full Relationships between Arctic sea ice drift and strength modelled by NEMO-LIM3.6
title_fullStr Relationships between Arctic sea ice drift and strength modelled by NEMO-LIM3.6
title_full_unstemmed Relationships between Arctic sea ice drift and strength modelled by NEMO-LIM3.6
title_sort relationships between arctic sea ice drift and strength modelled by nemo-lim3.6
publisher Copernicus GmbH
publishDate 2017
url http://hdl.handle.net/2078.1/192309
https://doi.org/10.5194/tc-11-2829-2017
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Sea ice
The Cryosphere
genre_facet Arctic
Arctic Ocean
Sea ice
The Cryosphere
op_source The Cryosphere, Vol. 11, p. 829-2846
op_relation boreal:192309
http://hdl.handle.net/2078.1/192309
doi:10.5194/tc-11-2829-2017
urn:ISSN:1994-0416
urn:EISSN:1994-0424
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5194/tc-11-2829-2017
container_title Biogeosciences
container_volume 18
container_issue 8
container_start_page 2649
op_container_end_page 2662
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