Topography-mediated transport of warm deep water across the continental shelf slope, East Antarctica ...
<!--!introduction!--> Warm Deep Water intrusion over the Antarctic continental shelves threatens the Antarctic ice-sheet stability by enhancing the basal melting of ice shelves. In East Antarctica, the Antarctic Slope Current (ASC), along with the Antarctic Slope Front (ASF), acts as a potenti...
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GFZ German Research Centre for Geosciences
2023
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Online Access: | https://dx.doi.org/10.57757/iugg23-0322 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016138 |
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ftdatacite:10.57757/iugg23-0322 2023-06-11T04:07:07+02:00 Topography-mediated transport of warm deep water across the continental shelf slope, East Antarctica ... Liu, Chengyan Wang, Zhaomin Liang, Xi Li, Xiang Li, Xichen Cheng, Chen Qi, Di 2023 https://dx.doi.org/10.57757/iugg23-0322 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016138 unknown GFZ German Research Centre for Geosciences Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Oral ConferencePaper Article 2023 ftdatacite https://doi.org/10.57757/iugg23-0322 2023-05-02T10:27:28Z <!--!introduction!--> Warm Deep Water intrusion over the Antarctic continental shelves threatens the Antarctic ice-sheet stability by enhancing the basal melting of ice shelves. In East Antarctica, the Antarctic Slope Current (ASC), along with the Antarctic Slope Front (ASF), acts as a potential vorticity barrier to prevent the warm modified Circumpolar Deep Water (mCDW) from ventilating the cold and fresh shelf. However, mCDW onshore transport is still observed within certain shelf regions, such as submarine troughs running perpendicular to the continental shelf. This study focuses on the dynamic mechanisms governing mCDW intrusion within a submarine trough over the fresh shelf regions, East Antarctica. Based on an idealized eddy-resolving coupled ocean-ice shelf model, two high resolution process-oriented numerical experiments are conducted to reveal the mechanisms responsible for the mCDW onshore transport. Three dynamic mechanisms governing cross-slope mCDW intrusion are identified: 1) the bottom ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ... Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica Ice Sheet Ice Shelf Ice Shelves DataCite Metadata Store (German National Library of Science and Technology) Antarctic East Antarctica The Antarctic |
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DataCite Metadata Store (German National Library of Science and Technology) |
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description |
<!--!introduction!--> Warm Deep Water intrusion over the Antarctic continental shelves threatens the Antarctic ice-sheet stability by enhancing the basal melting of ice shelves. In East Antarctica, the Antarctic Slope Current (ASC), along with the Antarctic Slope Front (ASF), acts as a potential vorticity barrier to prevent the warm modified Circumpolar Deep Water (mCDW) from ventilating the cold and fresh shelf. However, mCDW onshore transport is still observed within certain shelf regions, such as submarine troughs running perpendicular to the continental shelf. This study focuses on the dynamic mechanisms governing mCDW intrusion within a submarine trough over the fresh shelf regions, East Antarctica. Based on an idealized eddy-resolving coupled ocean-ice shelf model, two high resolution process-oriented numerical experiments are conducted to reveal the mechanisms responsible for the mCDW onshore transport. Three dynamic mechanisms governing cross-slope mCDW intrusion are identified: 1) the bottom ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ... |
format |
Article in Journal/Newspaper |
author |
Liu, Chengyan Wang, Zhaomin Liang, Xi Li, Xiang Li, Xichen Cheng, Chen Qi, Di |
spellingShingle |
Liu, Chengyan Wang, Zhaomin Liang, Xi Li, Xiang Li, Xichen Cheng, Chen Qi, Di Topography-mediated transport of warm deep water across the continental shelf slope, East Antarctica ... |
author_facet |
Liu, Chengyan Wang, Zhaomin Liang, Xi Li, Xiang Li, Xichen Cheng, Chen Qi, Di |
author_sort |
Liu, Chengyan |
title |
Topography-mediated transport of warm deep water across the continental shelf slope, East Antarctica ... |
title_short |
Topography-mediated transport of warm deep water across the continental shelf slope, East Antarctica ... |
title_full |
Topography-mediated transport of warm deep water across the continental shelf slope, East Antarctica ... |
title_fullStr |
Topography-mediated transport of warm deep water across the continental shelf slope, East Antarctica ... |
title_full_unstemmed |
Topography-mediated transport of warm deep water across the continental shelf slope, East Antarctica ... |
title_sort |
topography-mediated transport of warm deep water across the continental shelf slope, east antarctica ... |
publisher |
GFZ German Research Centre for Geosciences |
publishDate |
2023 |
url |
https://dx.doi.org/10.57757/iugg23-0322 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016138 |
geographic |
Antarctic East Antarctica The Antarctic |
geographic_facet |
Antarctic East Antarctica The Antarctic |
genre |
Antarc* Antarctic Antarctica East Antarctica Ice Sheet Ice Shelf Ice Shelves |
genre_facet |
Antarc* Antarctic Antarctica East Antarctica Ice Sheet Ice Shelf Ice Shelves |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.57757/iugg23-0322 |
_version_ |
1768379781043191808 |