Decadal variability of ice-shelf melting in the Amundsen Sea driven by sea-ice freshwater fluxes
The ice streams flowing into the Amundsen Sea, West Antarctica, are losing mass due to changes in oceanic basal melting of their floating ice shelves. Rapid ice-shelf melting is sustained by the delivery of warm Circumpolar Deep Water to the ice-shelf cavities, which is first supplied to the contine...
Published in: | Geophysical Research Letters |
---|---|
Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Geophysical Union
2024
|
Subjects: | |
Online Access: | http://nora.nerc.ac.uk/id/eprint/536808/ https://nora.nerc.ac.uk/id/eprint/536808/1/Geophysical%20Research%20Letters%20-%202024%20-%20Haigh%20-%20Decadal%20Variability%20of%20Ice%E2%80%90Shelf%20Melting%20in%20the%20Amundsen%20Sea%20Driven%20by.pdf https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2024GL108406 |
id |
ftnerc:oai:nora.nerc.ac.uk:536808 |
---|---|
record_format |
openpolar |
spelling |
ftnerc:oai:nora.nerc.ac.uk:536808 2024-06-09T07:38:17+00:00 Decadal variability of ice-shelf melting in the Amundsen Sea driven by sea-ice freshwater fluxes Haigh, Michael Holland, Paul R. 2024-05-08 text http://nora.nerc.ac.uk/id/eprint/536808/ https://nora.nerc.ac.uk/id/eprint/536808/1/Geophysical%20Research%20Letters%20-%202024%20-%20Haigh%20-%20Decadal%20Variability%20of%20Ice%E2%80%90Shelf%20Melting%20in%20the%20Amundsen%20Sea%20Driven%20by.pdf https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2024GL108406 en eng American Geophysical Union https://nora.nerc.ac.uk/id/eprint/536808/1/Geophysical%20Research%20Letters%20-%202024%20-%20Haigh%20-%20Decadal%20Variability%20of%20Ice%E2%80%90Shelf%20Melting%20in%20the%20Amundsen%20Sea%20Driven%20by.pdf Haigh, Michael orcid:0000-0001-9062-7613 Holland, Paul R. orcid:0000-0001-8370-289X . 2024 Decadal variability of ice-shelf melting in the Amundsen Sea driven by sea-ice freshwater fluxes. Geophysical Research Letters, 51 (9), e2024GL108406. 10, pp. https://doi.org/10.1029/2024GL108406 <https://doi.org/10.1029/2024GL108406> cc_by_4 Publication - Article PeerReviewed 2024 ftnerc https://doi.org/10.1029/2024GL108406 2024-05-15T14:16:28Z The ice streams flowing into the Amundsen Sea, West Antarctica, are losing mass due to changes in oceanic basal melting of their floating ice shelves. Rapid ice-shelf melting is sustained by the delivery of warm Circumpolar Deep Water to the ice-shelf cavities, which is first supplied to the continental shelf by an undercurrent that flows eastward along the shelf break. Temporal variability of this undercurrent controls ice-shelf basal melt variability. Recent work shows that on decadal timescales the undercurrent variability opposes surface wind variability. Using a regional model, we show that undercurrent variability is induced by sea-ice freshwater fluxes, particularly those north of the shelf break, which affect the cross-shelf break density gradient. This sea-ice variability is linked to tropical Pacific variability impacting atmospheric conditions over the Amundsen Sea. Ice-shelf melting also feeds back onto the undercurrent by affecting the on-shelf density, thereby influencing shelf-break density gradient anomalies. Article in Journal/Newspaper Amundsen Sea Antarc* Antarctica Ice Shelf Ice Shelves Sea ice West Antarctica Natural Environment Research Council: NERC Open Research Archive West Antarctica Amundsen Sea Pacific Geophysical Research Letters 51 9 |
institution |
Open Polar |
collection |
Natural Environment Research Council: NERC Open Research Archive |
op_collection_id |
ftnerc |
language |
English |
description |
The ice streams flowing into the Amundsen Sea, West Antarctica, are losing mass due to changes in oceanic basal melting of their floating ice shelves. Rapid ice-shelf melting is sustained by the delivery of warm Circumpolar Deep Water to the ice-shelf cavities, which is first supplied to the continental shelf by an undercurrent that flows eastward along the shelf break. Temporal variability of this undercurrent controls ice-shelf basal melt variability. Recent work shows that on decadal timescales the undercurrent variability opposes surface wind variability. Using a regional model, we show that undercurrent variability is induced by sea-ice freshwater fluxes, particularly those north of the shelf break, which affect the cross-shelf break density gradient. This sea-ice variability is linked to tropical Pacific variability impacting atmospheric conditions over the Amundsen Sea. Ice-shelf melting also feeds back onto the undercurrent by affecting the on-shelf density, thereby influencing shelf-break density gradient anomalies. |
format |
Article in Journal/Newspaper |
author |
Haigh, Michael Holland, Paul R. |
spellingShingle |
Haigh, Michael Holland, Paul R. Decadal variability of ice-shelf melting in the Amundsen Sea driven by sea-ice freshwater fluxes |
author_facet |
Haigh, Michael Holland, Paul R. |
author_sort |
Haigh, Michael |
title |
Decadal variability of ice-shelf melting in the Amundsen Sea driven by sea-ice freshwater fluxes |
title_short |
Decadal variability of ice-shelf melting in the Amundsen Sea driven by sea-ice freshwater fluxes |
title_full |
Decadal variability of ice-shelf melting in the Amundsen Sea driven by sea-ice freshwater fluxes |
title_fullStr |
Decadal variability of ice-shelf melting in the Amundsen Sea driven by sea-ice freshwater fluxes |
title_full_unstemmed |
Decadal variability of ice-shelf melting in the Amundsen Sea driven by sea-ice freshwater fluxes |
title_sort |
decadal variability of ice-shelf melting in the amundsen sea driven by sea-ice freshwater fluxes |
publisher |
American Geophysical Union |
publishDate |
2024 |
url |
http://nora.nerc.ac.uk/id/eprint/536808/ https://nora.nerc.ac.uk/id/eprint/536808/1/Geophysical%20Research%20Letters%20-%202024%20-%20Haigh%20-%20Decadal%20Variability%20of%20Ice%E2%80%90Shelf%20Melting%20in%20the%20Amundsen%20Sea%20Driven%20by.pdf https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2024GL108406 |
geographic |
West Antarctica Amundsen Sea Pacific |
geographic_facet |
West Antarctica Amundsen Sea Pacific |
genre |
Amundsen Sea Antarc* Antarctica Ice Shelf Ice Shelves Sea ice West Antarctica |
genre_facet |
Amundsen Sea Antarc* Antarctica Ice Shelf Ice Shelves Sea ice West Antarctica |
op_relation |
https://nora.nerc.ac.uk/id/eprint/536808/1/Geophysical%20Research%20Letters%20-%202024%20-%20Haigh%20-%20Decadal%20Variability%20of%20Ice%E2%80%90Shelf%20Melting%20in%20the%20Amundsen%20Sea%20Driven%20by.pdf Haigh, Michael orcid:0000-0001-9062-7613 Holland, Paul R. orcid:0000-0001-8370-289X . 2024 Decadal variability of ice-shelf melting in the Amundsen Sea driven by sea-ice freshwater fluxes. Geophysical Research Letters, 51 (9), e2024GL108406. 10, pp. https://doi.org/10.1029/2024GL108406 <https://doi.org/10.1029/2024GL108406> |
op_rights |
cc_by_4 |
op_doi |
https://doi.org/10.1029/2024GL108406 |
container_title |
Geophysical Research Letters |
container_volume |
51 |
container_issue |
9 |
_version_ |
1801371385329614848 |