Variability of Inflowing Current Into the Dotson Ice Shelf and Its Cause in the Amundsen Sea
Abstract The inflow of warm and salty Circumpolar Deep Water affects the melting of the ice shelf on the Amundsen Sea, a significant contributor to global sea level rise. Multi‐year mooring data (2014–2016 and 2018–2020) from the front of the Dotson Ice Shelf show the modified Circumpolar Deep Water...
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Online Access: | https://doi.org/10.1029/2023GL105404 https://doaj.org/article/229c8b9ea3bf4beba6aa221f7f7fbee6 |
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ftdoajarticles:oai:doaj.org/article:229c8b9ea3bf4beba6aa221f7f7fbee6 2024-09-15T17:38:58+00:00 Variability of Inflowing Current Into the Dotson Ice Shelf and Its Cause in the Amundsen Sea Heewon Yang Tae‐Wan Kim Yeonggi Kim Jaeill Yoo Jisoo Park Yang‐Ki Cho 2024-02-01T00:00:00Z https://doi.org/10.1029/2023GL105404 https://doaj.org/article/229c8b9ea3bf4beba6aa221f7f7fbee6 EN eng Wiley https://doi.org/10.1029/2023GL105404 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL105404 https://doaj.org/article/229c8b9ea3bf4beba6aa221f7f7fbee6 Geophysical Research Letters, Vol 51, Iss 3, Pp n/a-n/a (2024) Amundsen Sea Dotson Ice Shelf Circumpolar Deep Water ocean surface stress curl Geophysics. Cosmic physics QC801-809 article 2024 ftdoajarticles https://doi.org/10.1029/2023GL105404 2024-08-05T17:49:23Z Abstract The inflow of warm and salty Circumpolar Deep Water affects the melting of the ice shelf on the Amundsen Sea, a significant contributor to global sea level rise. Multi‐year mooring data (2014–2016 and 2018–2020) from the front of the Dotson Ice Shelf show the modified Circumpolar Deep Water layer was thicker during 2018–2020 than during 2014–2016. During 2014–2016, Ocean surface stress curl influenced the barotropic process and strengthened southward velocity, while during 2018–2020, it caused lift and downwelling of thermocline depth, increasing the impact of the baroclinic process in ocean circulation. The heat transport to the ice shelf during 2018–2020 (57.42 MW m−1) was half as much as it was during 2014–2016 (111.06 MW m−1) due to a weaker lower layer current. The difference in ocean circulation between two periods, caused by a difference in warm layer thickness, ultimately impacts the heat transport entering the ice shelf cavity. Article in Journal/Newspaper Amundsen Sea Dotson Ice Shelf Ice Shelf Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 51 3 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Amundsen Sea Dotson Ice Shelf Circumpolar Deep Water ocean surface stress curl Geophysics. Cosmic physics QC801-809 |
spellingShingle |
Amundsen Sea Dotson Ice Shelf Circumpolar Deep Water ocean surface stress curl Geophysics. Cosmic physics QC801-809 Heewon Yang Tae‐Wan Kim Yeonggi Kim Jaeill Yoo Jisoo Park Yang‐Ki Cho Variability of Inflowing Current Into the Dotson Ice Shelf and Its Cause in the Amundsen Sea |
topic_facet |
Amundsen Sea Dotson Ice Shelf Circumpolar Deep Water ocean surface stress curl Geophysics. Cosmic physics QC801-809 |
description |
Abstract The inflow of warm and salty Circumpolar Deep Water affects the melting of the ice shelf on the Amundsen Sea, a significant contributor to global sea level rise. Multi‐year mooring data (2014–2016 and 2018–2020) from the front of the Dotson Ice Shelf show the modified Circumpolar Deep Water layer was thicker during 2018–2020 than during 2014–2016. During 2014–2016, Ocean surface stress curl influenced the barotropic process and strengthened southward velocity, while during 2018–2020, it caused lift and downwelling of thermocline depth, increasing the impact of the baroclinic process in ocean circulation. The heat transport to the ice shelf during 2018–2020 (57.42 MW m−1) was half as much as it was during 2014–2016 (111.06 MW m−1) due to a weaker lower layer current. The difference in ocean circulation between two periods, caused by a difference in warm layer thickness, ultimately impacts the heat transport entering the ice shelf cavity. |
format |
Article in Journal/Newspaper |
author |
Heewon Yang Tae‐Wan Kim Yeonggi Kim Jaeill Yoo Jisoo Park Yang‐Ki Cho |
author_facet |
Heewon Yang Tae‐Wan Kim Yeonggi Kim Jaeill Yoo Jisoo Park Yang‐Ki Cho |
author_sort |
Heewon Yang |
title |
Variability of Inflowing Current Into the Dotson Ice Shelf and Its Cause in the Amundsen Sea |
title_short |
Variability of Inflowing Current Into the Dotson Ice Shelf and Its Cause in the Amundsen Sea |
title_full |
Variability of Inflowing Current Into the Dotson Ice Shelf and Its Cause in the Amundsen Sea |
title_fullStr |
Variability of Inflowing Current Into the Dotson Ice Shelf and Its Cause in the Amundsen Sea |
title_full_unstemmed |
Variability of Inflowing Current Into the Dotson Ice Shelf and Its Cause in the Amundsen Sea |
title_sort |
variability of inflowing current into the dotson ice shelf and its cause in the amundsen sea |
publisher |
Wiley |
publishDate |
2024 |
url |
https://doi.org/10.1029/2023GL105404 https://doaj.org/article/229c8b9ea3bf4beba6aa221f7f7fbee6 |
genre |
Amundsen Sea Dotson Ice Shelf Ice Shelf |
genre_facet |
Amundsen Sea Dotson Ice Shelf Ice Shelf |
op_source |
Geophysical Research Letters, Vol 51, Iss 3, Pp n/a-n/a (2024) |
op_relation |
https://doi.org/10.1029/2023GL105404 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL105404 https://doaj.org/article/229c8b9ea3bf4beba6aa221f7f7fbee6 |
op_doi |
https://doi.org/10.1029/2023GL105404 |
container_title |
Geophysical Research Letters |
container_volume |
51 |
container_issue |
3 |
_version_ |
1810476536726290432 |