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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Main Authors: Van Achter, Guillian, Fichefet, Thierry, Goosse, Hugues, Pelletier, Charles, Haubner, Konstanze, Pattyn, Frank
Format: Article in Journal/Newspaper
Language:English
Published: 2023
Subjects:
Online Access: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
id ftunivbruxelles:oai:dipot.ulb.ac.be:2013/357336
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spelling 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
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