Sources and Pathways of Glacial Meltwater in the Bellingshausen Sea, Antarctica

Abstract Meltwater content and pathways determine the impact of Antarctica's melting ice shelves on ocean circulation and climate. Using ocean glider observations, we quantify meltwater distribution and transport within the Bellingshausen Sea's Belgica Trough. Meltwater is present at diffe...

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Published in:Geophysical Research Letters
Main Authors: Peter M. F. Sheehan, Karen J. Heywood, Andrew F. Thompson, M. Mar Flexas, Michael P. Schodlok
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:https://doi.org/10.1029/2023GL102785
https://doaj.org/article/5919eafcb88c4acaa557a51d297b2202
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spelling ftdoajarticles:oai:doaj.org/article:5919eafcb88c4acaa557a51d297b2202 2024-09-15T17:48:10+00:00 Sources and Pathways of Glacial Meltwater in the Bellingshausen Sea, Antarctica Peter M. F. Sheehan Karen J. Heywood Andrew F. Thompson M. Mar Flexas Michael P. Schodlok 2023-07-01T00:00:00Z https://doi.org/10.1029/2023GL102785 https://doaj.org/article/5919eafcb88c4acaa557a51d297b2202 EN eng Wiley https://doi.org/10.1029/2023GL102785 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL102785 https://doaj.org/article/5919eafcb88c4acaa557a51d297b2202 Geophysical Research Letters, Vol 50, Iss 14, Pp n/a-n/a (2023) Antarctica Bellingshausen Sea meltwater Geophysics. Cosmic physics QC801-809 article 2023 ftdoajarticles https://doi.org/10.1029/2023GL102785 2024-08-05T17:49:23Z Abstract Meltwater content and pathways determine the impact of Antarctica's melting ice shelves on ocean circulation and climate. Using ocean glider observations, we quantify meltwater distribution and transport within the Bellingshausen Sea's Belgica Trough. Meltwater is present at different densities and with different turbidities: both are indicative of a layer's ice shelf of origin. To investigate how ice‐shelf origin separates meltwater into different export pathways, we compare these observations with high‐resolution tracer‐release model simulations. Meltwater filaments branch off the Antarctic Coastal Current into the southwestern trough. Meltwater also enters the Belgica Trough in the northwest via an extended western pathway, hence the greater observed southward (0.50 mSv) than northward (0.17 mSv) meltwater transport. Together, the observations and simulations reveal meltwater retention within a cyclonic in‐trough gyre, which has the potential to promote climactically important feedbacks on circulation and future melting. Article in Journal/Newspaper Antarc* Antarctic Antarctica Bellingshausen Sea Ice Shelf Ice Shelves Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 50 14
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Antarctica
Bellingshausen Sea
meltwater
Geophysics. Cosmic physics
QC801-809
spellingShingle Antarctica
Bellingshausen Sea
meltwater
Geophysics. Cosmic physics
QC801-809
Peter M. F. Sheehan
Karen J. Heywood
Andrew F. Thompson
M. Mar Flexas
Michael P. Schodlok
Sources and Pathways of Glacial Meltwater in the Bellingshausen Sea, Antarctica
topic_facet Antarctica
Bellingshausen Sea
meltwater
Geophysics. Cosmic physics
QC801-809
description Abstract Meltwater content and pathways determine the impact of Antarctica's melting ice shelves on ocean circulation and climate. Using ocean glider observations, we quantify meltwater distribution and transport within the Bellingshausen Sea's Belgica Trough. Meltwater is present at different densities and with different turbidities: both are indicative of a layer's ice shelf of origin. To investigate how ice‐shelf origin separates meltwater into different export pathways, we compare these observations with high‐resolution tracer‐release model simulations. Meltwater filaments branch off the Antarctic Coastal Current into the southwestern trough. Meltwater also enters the Belgica Trough in the northwest via an extended western pathway, hence the greater observed southward (0.50 mSv) than northward (0.17 mSv) meltwater transport. Together, the observations and simulations reveal meltwater retention within a cyclonic in‐trough gyre, which has the potential to promote climactically important feedbacks on circulation and future melting.
format Article in Journal/Newspaper
author Peter M. F. Sheehan
Karen J. Heywood
Andrew F. Thompson
M. Mar Flexas
Michael P. Schodlok
author_facet Peter M. F. Sheehan
Karen J. Heywood
Andrew F. Thompson
M. Mar Flexas
Michael P. Schodlok
author_sort Peter M. F. Sheehan
title Sources and Pathways of Glacial Meltwater in the Bellingshausen Sea, Antarctica
title_short Sources and Pathways of Glacial Meltwater in the Bellingshausen Sea, Antarctica
title_full Sources and Pathways of Glacial Meltwater in the Bellingshausen Sea, Antarctica
title_fullStr Sources and Pathways of Glacial Meltwater in the Bellingshausen Sea, Antarctica
title_full_unstemmed Sources and Pathways of Glacial Meltwater in the Bellingshausen Sea, Antarctica
title_sort sources and pathways of glacial meltwater in the bellingshausen sea, antarctica
publisher Wiley
publishDate 2023
url https://doi.org/10.1029/2023GL102785
https://doaj.org/article/5919eafcb88c4acaa557a51d297b2202
genre Antarc*
Antarctic
Antarctica
Bellingshausen Sea
Ice Shelf
Ice Shelves
genre_facet Antarc*
Antarctic
Antarctica
Bellingshausen Sea
Ice Shelf
Ice Shelves
op_source Geophysical Research Letters, Vol 50, Iss 14, Pp n/a-n/a (2023)
op_relation https://doi.org/10.1029/2023GL102785
https://doaj.org/toc/0094-8276
https://doaj.org/toc/1944-8007
1944-8007
0094-8276
doi:10.1029/2023GL102785
https://doaj.org/article/5919eafcb88c4acaa557a51d297b2202
op_doi https://doi.org/10.1029/2023GL102785
container_title Geophysical Research Letters
container_volume 50
container_issue 14
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