Decadal Ocean Forcing and Antarctic Ice Sheet Response: Lessons from the Amundsen Sea
Mass loss from the Antarctic Ice Sheet is driven by changes at the marine margins. In the Amundsen Sea, thinning of the ice shelves has allowed the outlet glaciers to accelerate and thin, resulting in inland migration of their grounding lines. The ultimate driver is often assumed to be ocean warming...
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ftdoajarticles:oai:doaj.org/article:e05c89ccd58444708892ba96514f6e73 2023-05-15T13:23:33+02:00 Decadal Ocean Forcing and Antarctic Ice Sheet Response: Lessons from the Amundsen Sea Adrian Jenkins Pierre Dutrieux Stan Jacobs Eric J. Steig G. Hilmar Gudmundsson James Smith Karen J. Heywood 2016-12-01T00:00:00Z https://doi.org/10.5670/oceanog.2016.103 https://doaj.org/article/e05c89ccd58444708892ba96514f6e73 EN eng The Oceanography Society https://tos.org/oceanography/assets/docs/29-4_jenkins.pdf https://doaj.org/toc/1042-8275 doi:10.5670/oceanog.2016.103 1042-8275 https://doaj.org/article/e05c89ccd58444708892ba96514f6e73 Oceanography, Vol 29, Iss 4, Pp 106-117 (2016) Antarctic Ice Sheet Amundsen Sea ice shelves ocean warming Oceanography GC1-1581 article 2016 ftdoajarticles https://doi.org/10.5670/oceanog.2016.103 2022-12-31T03:12:01Z Mass loss from the Antarctic Ice Sheet is driven by changes at the marine margins. In the Amundsen Sea, thinning of the ice shelves has allowed the outlet glaciers to accelerate and thin, resulting in inland migration of their grounding lines. The ultimate driver is often assumed to be ocean warming, but the recent record of ocean temperature is dominated by decadal variability rather than a trend. The distribution of water masses on the Amundsen Sea continental shelf is particularly sensitive to atmospheric forcing, while the regional atmospheric circulation is highly variable, at least in part because of the impact of tropical variability. Changes in atmospheric circulation force changes in ice shelf melting, which drive step-wise movement of the grounding line between localized high points on the bed. When the grounding line is located on a high point, outlet glacier flow is sensitive to atmosphere-ocean variability, but once retreat or advance to the next high point has been triggered, ocean circulation and melt rate changes associated with the evolution in geometry of the sub-ice-shelf cavity dominate, and the sensitivity to atmospheric forcing is greatly reduced. Article in Journal/Newspaper Amundsen Sea Antarc* Antarctic Ice Sheet Ice Shelf Ice Shelves Sea ice Directory of Open Access Journals: DOAJ Articles Amundsen Sea Antarctic The Antarctic Oceanography 29 4 106 117 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Antarctic Ice Sheet Amundsen Sea ice shelves ocean warming Oceanography GC1-1581 |
spellingShingle |
Antarctic Ice Sheet Amundsen Sea ice shelves ocean warming Oceanography GC1-1581 Adrian Jenkins Pierre Dutrieux Stan Jacobs Eric J. Steig G. Hilmar Gudmundsson James Smith Karen J. Heywood Decadal Ocean Forcing and Antarctic Ice Sheet Response: Lessons from the Amundsen Sea |
topic_facet |
Antarctic Ice Sheet Amundsen Sea ice shelves ocean warming Oceanography GC1-1581 |
description |
Mass loss from the Antarctic Ice Sheet is driven by changes at the marine margins. In the Amundsen Sea, thinning of the ice shelves has allowed the outlet glaciers to accelerate and thin, resulting in inland migration of their grounding lines. The ultimate driver is often assumed to be ocean warming, but the recent record of ocean temperature is dominated by decadal variability rather than a trend. The distribution of water masses on the Amundsen Sea continental shelf is particularly sensitive to atmospheric forcing, while the regional atmospheric circulation is highly variable, at least in part because of the impact of tropical variability. Changes in atmospheric circulation force changes in ice shelf melting, which drive step-wise movement of the grounding line between localized high points on the bed. When the grounding line is located on a high point, outlet glacier flow is sensitive to atmosphere-ocean variability, but once retreat or advance to the next high point has been triggered, ocean circulation and melt rate changes associated with the evolution in geometry of the sub-ice-shelf cavity dominate, and the sensitivity to atmospheric forcing is greatly reduced. |
format |
Article in Journal/Newspaper |
author |
Adrian Jenkins Pierre Dutrieux Stan Jacobs Eric J. Steig G. Hilmar Gudmundsson James Smith Karen J. Heywood |
author_facet |
Adrian Jenkins Pierre Dutrieux Stan Jacobs Eric J. Steig G. Hilmar Gudmundsson James Smith Karen J. Heywood |
author_sort |
Adrian Jenkins |
title |
Decadal Ocean Forcing and Antarctic Ice Sheet Response: Lessons from the Amundsen Sea |
title_short |
Decadal Ocean Forcing and Antarctic Ice Sheet Response: Lessons from the Amundsen Sea |
title_full |
Decadal Ocean Forcing and Antarctic Ice Sheet Response: Lessons from the Amundsen Sea |
title_fullStr |
Decadal Ocean Forcing and Antarctic Ice Sheet Response: Lessons from the Amundsen Sea |
title_full_unstemmed |
Decadal Ocean Forcing and Antarctic Ice Sheet Response: Lessons from the Amundsen Sea |
title_sort |
decadal ocean forcing and antarctic ice sheet response: lessons from the amundsen sea |
publisher |
The Oceanography Society |
publishDate |
2016 |
url |
https://doi.org/10.5670/oceanog.2016.103 https://doaj.org/article/e05c89ccd58444708892ba96514f6e73 |
geographic |
Amundsen Sea Antarctic The Antarctic |
geographic_facet |
Amundsen Sea Antarctic The Antarctic |
genre |
Amundsen Sea Antarc* Antarctic Ice Sheet Ice Shelf Ice Shelves Sea ice |
genre_facet |
Amundsen Sea Antarc* Antarctic Ice Sheet Ice Shelf Ice Shelves Sea ice |
op_source |
Oceanography, Vol 29, Iss 4, Pp 106-117 (2016) |
op_relation |
https://tos.org/oceanography/assets/docs/29-4_jenkins.pdf https://doaj.org/toc/1042-8275 doi:10.5670/oceanog.2016.103 1042-8275 https://doaj.org/article/e05c89ccd58444708892ba96514f6e73 |
op_doi |
https://doi.org/10.5670/oceanog.2016.103 |
container_title |
Oceanography |
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29 |
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4 |
container_start_page |
106 |
op_container_end_page |
117 |
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