Ocean–Ice Sheet Coupling in the Totten Glacier Area, East Antarctica: Analysis of the Feedbacks and Their Response to a Sudden Ocean Warming
We coupled together high-resolution versions of the ocean–sea ice model NEMO and the ice sheet model BISICLES configured to the Totten Glacier area and ran a series of simulations over the recent past (1995–2014) and under warming conditions (2081–2100; SSP4-4.5) with NEMO in stand-alone mode and wi...
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ftunivbruxelles:oai:dipot.ulb.ac.be:2013/357336 2024-04-28T08:02:21+00:00 Ocean–Ice Sheet Coupling in the Totten Glacier Area, East Antarctica: Analysis of the Feedbacks and Their Response to a Sudden Ocean Warming Van Achter, Guillian Fichefet, Thierry Goosse, Hugues Pelletier, Charles Haubner, Konstanze Pattyn, Frank 2023-04-01 1 full-text file(s): application/pdf http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/357336 https://dipot.ulb.ac.be/dspace/bitstream/2013/357336/3/VanAchter2023_Geosciences.pdf en eng uri/info:doi/10.3390/geosciences13040106 uri/info:pii/geosciences13040106 uri/info:scp/85154045072 https://dipot.ulb.ac.be/dspace/bitstream/2013/357336/3/VanAchter2023_Geosciences.pdf http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/357336 1 full-text file(s): info:eu-repo/semantics/openAccess Geosciences (Switzerland), 13 (4 Sciences exactes et naturelles basal melt rates NEMO–BISICLES coupling ocean–ice shelf interactions info:eu-repo/semantics/article info:ulb-repo/semantics/articlePeerReview info:ulb-repo/semantics/openurl/article 2023 ftunivbruxelles 2024-04-10T00:14:40Z We coupled together high-resolution versions of the ocean–sea ice model NEMO and the ice sheet model BISICLES configured to the Totten Glacier area and ran a series of simulations over the recent past (1995–2014) and under warming conditions (2081–2100; SSP4-4.5) with NEMO in stand-alone mode and with the coupled model to assess the effects of the coupling. During the recent past, the ocean–ice sheet coupling has increased the time-averaged value of the basal melt rate in both the Totten and Moscow University ice shelf cavities by 6.7% and 14.2%, respectively. The relationship between the changes in ice shelf thickness and ice shelf basal melt rate suggests that the effect of the coupling is not a linear response to the melt rate but rather a more complex response, driven partly by the dynamical component of the ice sheet model. The response of the ice sheet–ocean coupling due to the ocean warming is a 10% and 3% basal melt rate decrease in the Totten and Moscow University ice shelf cavities, respectively. This indicates that the ocean–ice sheet coupling under climate warming conditions dampens the basal melt rates. Our study highlights the importance of incorporating ocean–ice sheet coupling in climate simulations, even over short time periods. SCOPUS: ar.j info:eu-repo/semantics/published Article in Journal/Newspaper Antarc* Antarctica East Antarctica Ice Sheet Ice Shelf Moscow University Ice Shelf Sea ice Totten Glacier DI-fusion : dépôt institutionnel de l'Université libre de Bruxelles (ULB) |
institution |
Open Polar |
collection |
DI-fusion : dépôt institutionnel de l'Université libre de Bruxelles (ULB) |
op_collection_id |
ftunivbruxelles |
language |
English |
topic |
Sciences exactes et naturelles basal melt rates NEMO–BISICLES coupling ocean–ice shelf interactions |
spellingShingle |
Sciences exactes et naturelles basal melt rates NEMO–BISICLES coupling ocean–ice shelf interactions Van Achter, Guillian Fichefet, Thierry Goosse, Hugues Pelletier, Charles Haubner, Konstanze Pattyn, Frank Ocean–Ice Sheet Coupling in the Totten Glacier Area, East Antarctica: Analysis of the Feedbacks and Their Response to a Sudden Ocean Warming |
topic_facet |
Sciences exactes et naturelles basal melt rates NEMO–BISICLES coupling ocean–ice shelf interactions |
description |
We coupled together high-resolution versions of the ocean–sea ice model NEMO and the ice sheet model BISICLES configured to the Totten Glacier area and ran a series of simulations over the recent past (1995–2014) and under warming conditions (2081–2100; SSP4-4.5) with NEMO in stand-alone mode and with the coupled model to assess the effects of the coupling. During the recent past, the ocean–ice sheet coupling has increased the time-averaged value of the basal melt rate in both the Totten and Moscow University ice shelf cavities by 6.7% and 14.2%, respectively. The relationship between the changes in ice shelf thickness and ice shelf basal melt rate suggests that the effect of the coupling is not a linear response to the melt rate but rather a more complex response, driven partly by the dynamical component of the ice sheet model. The response of the ice sheet–ocean coupling due to the ocean warming is a 10% and 3% basal melt rate decrease in the Totten and Moscow University ice shelf cavities, respectively. This indicates that the ocean–ice sheet coupling under climate warming conditions dampens the basal melt rates. Our study highlights the importance of incorporating ocean–ice sheet coupling in climate simulations, even over short time periods. SCOPUS: ar.j info:eu-repo/semantics/published |
format |
Article in Journal/Newspaper |
author |
Van Achter, Guillian Fichefet, Thierry Goosse, Hugues Pelletier, Charles Haubner, Konstanze Pattyn, Frank |
author_facet |
Van Achter, Guillian Fichefet, Thierry Goosse, Hugues Pelletier, Charles Haubner, Konstanze Pattyn, Frank |
author_sort |
Van Achter, Guillian |
title |
Ocean–Ice Sheet Coupling in the Totten Glacier Area, East Antarctica: Analysis of the Feedbacks and Their Response to a Sudden Ocean Warming |
title_short |
Ocean–Ice Sheet Coupling in the Totten Glacier Area, East Antarctica: Analysis of the Feedbacks and Their Response to a Sudden Ocean Warming |
title_full |
Ocean–Ice Sheet Coupling in the Totten Glacier Area, East Antarctica: Analysis of the Feedbacks and Their Response to a Sudden Ocean Warming |
title_fullStr |
Ocean–Ice Sheet Coupling in the Totten Glacier Area, East Antarctica: Analysis of the Feedbacks and Their Response to a Sudden Ocean Warming |
title_full_unstemmed |
Ocean–Ice Sheet Coupling in the Totten Glacier Area, East Antarctica: Analysis of the Feedbacks and Their Response to a Sudden Ocean Warming |
title_sort |
ocean–ice sheet coupling in the totten glacier area, east antarctica: analysis of the feedbacks and their response to a sudden ocean warming |
publishDate |
2023 |
url |
http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/357336 https://dipot.ulb.ac.be/dspace/bitstream/2013/357336/3/VanAchter2023_Geosciences.pdf |
genre |
Antarc* Antarctica East Antarctica Ice Sheet Ice Shelf Moscow University Ice Shelf Sea ice Totten Glacier |
genre_facet |
Antarc* Antarctica East Antarctica Ice Sheet Ice Shelf Moscow University Ice Shelf Sea ice Totten Glacier |
op_source |
Geosciences (Switzerland), 13 (4 |
op_relation |
uri/info:doi/10.3390/geosciences13040106 uri/info:pii/geosciences13040106 uri/info:scp/85154045072 https://dipot.ulb.ac.be/dspace/bitstream/2013/357336/3/VanAchter2023_Geosciences.pdf http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/357336 |
op_rights |
1 full-text file(s): info:eu-repo/semantics/openAccess |
_version_ |
1797573742250950656 |