The Antarctic Coastal Current in the Bellingshausen Sea

The ice shelves of the West Antarctic Ice Sheet experience basal melting induced by underlying warm, salty Circumpolar Deep Water. Basal meltwater, along with runoff from ice sheets, supplies fresh buoyant water to a circulation feature near the coast, the Antarctic Coastal Current (AACC). The forma...

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Published in:The Cryosphere
Main Authors: Schubert, Ryan, Thompson, Andrew F., Speer, Kevin, Schulze Chretien, Lena, Bebieva, Yana
Format: Article in Journal/Newspaper
Language:unknown
Published: European Geosciences Union 2021
Subjects:
Online Access:https://doi.org/10.5194/tc-15-4179-2021
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spelling ftcaltechauth:oai:authors.library.caltech.edu:2ytpg-9qv85 2024-09-15T17:34:18+00:00 The Antarctic Coastal Current in the Bellingshausen Sea Schubert, Ryan Thompson, Andrew F. Speer, Kevin Schulze Chretien, Lena Bebieva, Yana 2021-09 https://doi.org/10.5194/tc-15-4179-2021 unknown European Geosciences Union https://meop.net/database/meop-databases/density-of-data.html https://doi.org/10.5194/tc-15-4179-2021 oai:authors.library.caltech.edu:2ytpg-9qv85 eprintid:111273 resolverid:CaltechAUTHORS:20211007-223111495 info:eu-repo/semantics/openAccess Other Cryosphere, 15(9), 4179-4199, (2021-09) info:eu-repo/semantics/article 2021 ftcaltechauth https://doi.org/10.5194/tc-15-4179-2021 2024-08-06T15:35:02Z The ice shelves of the West Antarctic Ice Sheet experience basal melting induced by underlying warm, salty Circumpolar Deep Water. Basal meltwater, along with runoff from ice sheets, supplies fresh buoyant water to a circulation feature near the coast, the Antarctic Coastal Current (AACC). The formation, structure, and coherence of the AACC has been well documented along the West Antarctic Peninsula (WAP). Observations from instrumented seals collected in the Bellingshausen Sea offer extensive hydrographic coverage throughout the year, providing evidence of the continuation of the westward flowing AACC from the WAP towards the Amundsen Sea. The observations reported here demonstrate that the coastal boundary current enters the eastern Bellingshausen Sea from the WAP and flows westward along the face of multiple ice shelves, including the westernmost Abbot Ice Shelf. The presence of the AACC in the western Bellingshausen Sea has implications for the export of water properties into the eastern Amundsen Sea, which we suggest may occur through multiple pathways, either along the coast or along the continental shelf break. The temperature, salinity, and density structure of the current indicates an increase in baroclinic transport as the AACC flows from the east to the west, and as it entrains meltwater from the ice shelves in the Bellingshausen Sea. The AACC acts as a mechanism to transport meltwater out of the Bellingshausen Sea and into the Amundsen and Ross seas, with the potential to impact, respectively, basal melt rates and bottom water formation in these regions. © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Received: 04 Feb 2021 – Discussion started: 19 Feb 2021 – Revised: 20 Jul 2021 – Accepted: 21 Jul 2021 – Published: 01 Sep 2021. We gratefully acknowledge all of the scientists who have contributed to the MEOP project through their seal tagging and data processing efforts. In particular, we thank Fabien Roquet, who assisted with processing of the ... Article in Journal/Newspaper Abbot Ice Shelf Amundsen Sea Antarc* Antarctic Antarctic Peninsula Bellingshausen Sea Ice Sheet Ice Shelf Ice Shelves Caltech Authors (California Institute of Technology) The Cryosphere 15 9 4179 4199
institution Open Polar
collection Caltech Authors (California Institute of Technology)
op_collection_id ftcaltechauth
language unknown
description The ice shelves of the West Antarctic Ice Sheet experience basal melting induced by underlying warm, salty Circumpolar Deep Water. Basal meltwater, along with runoff from ice sheets, supplies fresh buoyant water to a circulation feature near the coast, the Antarctic Coastal Current (AACC). The formation, structure, and coherence of the AACC has been well documented along the West Antarctic Peninsula (WAP). Observations from instrumented seals collected in the Bellingshausen Sea offer extensive hydrographic coverage throughout the year, providing evidence of the continuation of the westward flowing AACC from the WAP towards the Amundsen Sea. The observations reported here demonstrate that the coastal boundary current enters the eastern Bellingshausen Sea from the WAP and flows westward along the face of multiple ice shelves, including the westernmost Abbot Ice Shelf. The presence of the AACC in the western Bellingshausen Sea has implications for the export of water properties into the eastern Amundsen Sea, which we suggest may occur through multiple pathways, either along the coast or along the continental shelf break. The temperature, salinity, and density structure of the current indicates an increase in baroclinic transport as the AACC flows from the east to the west, and as it entrains meltwater from the ice shelves in the Bellingshausen Sea. The AACC acts as a mechanism to transport meltwater out of the Bellingshausen Sea and into the Amundsen and Ross seas, with the potential to impact, respectively, basal melt rates and bottom water formation in these regions. © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Received: 04 Feb 2021 – Discussion started: 19 Feb 2021 – Revised: 20 Jul 2021 – Accepted: 21 Jul 2021 – Published: 01 Sep 2021. We gratefully acknowledge all of the scientists who have contributed to the MEOP project through their seal tagging and data processing efforts. In particular, we thank Fabien Roquet, who assisted with processing of the ...
format Article in Journal/Newspaper
author Schubert, Ryan
Thompson, Andrew F.
Speer, Kevin
Schulze Chretien, Lena
Bebieva, Yana
spellingShingle Schubert, Ryan
Thompson, Andrew F.
Speer, Kevin
Schulze Chretien, Lena
Bebieva, Yana
The Antarctic Coastal Current in the Bellingshausen Sea
author_facet Schubert, Ryan
Thompson, Andrew F.
Speer, Kevin
Schulze Chretien, Lena
Bebieva, Yana
author_sort Schubert, Ryan
title The Antarctic Coastal Current in the Bellingshausen Sea
title_short The Antarctic Coastal Current in the Bellingshausen Sea
title_full The Antarctic Coastal Current in the Bellingshausen Sea
title_fullStr The Antarctic Coastal Current in the Bellingshausen Sea
title_full_unstemmed The Antarctic Coastal Current in the Bellingshausen Sea
title_sort antarctic coastal current in the bellingshausen sea
publisher European Geosciences Union
publishDate 2021
url https://doi.org/10.5194/tc-15-4179-2021
genre Abbot Ice Shelf
Amundsen Sea
Antarc*
Antarctic
Antarctic Peninsula
Bellingshausen Sea
Ice Sheet
Ice Shelf
Ice Shelves
genre_facet Abbot Ice Shelf
Amundsen Sea
Antarc*
Antarctic
Antarctic Peninsula
Bellingshausen Sea
Ice Sheet
Ice Shelf
Ice Shelves
op_source Cryosphere, 15(9), 4179-4199, (2021-09)
op_relation https://meop.net/database/meop-databases/density-of-data.html
https://doi.org/10.5194/tc-15-4179-2021
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Other
op_doi https://doi.org/10.5194/tc-15-4179-2021
container_title The Cryosphere
container_volume 15
container_issue 9
container_start_page 4179
op_container_end_page 4199
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