Enhanced upwelling of Antarctic Bottom Water by topographic interaction of water mass interfaces ...
<!--!introduction!--> The lower cell of the meridional overturning circulation (MOC) is sourced by dense Antarctic Bottom Water (AABW), which forms and sinks around Antarctica and subsequently fills the abyssal ocean. For the MOC to ‘overturn’, these dense waters must upwell through mixing wit...
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GFZ German Research Centre for Geosciences
2023
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ftdatacite:10.57757/iugg23-1573 2023-07-23T04:15:51+02:00 Enhanced upwelling of Antarctic Bottom Water by topographic interaction of water mass interfaces ... Baker, Lois Mashayek, Ali Naveira Garabato, Alberto 2023 https://dx.doi.org/10.57757/iugg23-1573 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018033 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 Article ConferencePaper Oral 2023 ftdatacite https://doi.org/10.57757/iugg23-1573 2023-07-03T16:18:40Z <!--!introduction!--> The lower cell of the meridional overturning circulation (MOC) is sourced by dense Antarctic Bottom Water (AABW), which forms and sinks around Antarctica and subsequently fills the abyssal ocean. For the MOC to ‘overturn’, these dense waters must upwell through mixing with lighter waters above. Here, we investigate the processes underpinning such mixing, and the resulting water mass transformation, using an observationally forced, high-resolution numerical model of the Drake Passage in the Southern Ocean. In the Drake Passage, the mixing of dense AABW formed in the Weddell Sea with lighter deep waters transported from the Pacific Ocean by the Antarctic Circumpolar Current is catalysed by energetic flows impinging on rough topography. We find that multiple topographic interaction processes act to facilitate mixing of the two water masses, ultimately resulting in upwelling of waters with neutral density greater 28.19 kg m -3 , and downwelling of the lighter waters above. In ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ... Conference Object Antarc* Antarctic Antarctica Drake Passage Southern Ocean Weddell Sea DataCite Metadata Store (German National Library of Science and Technology) Antarctic Southern Ocean The Antarctic Weddell Sea Drake Passage Pacific Weddell |
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DataCite Metadata Store (German National Library of Science and Technology) |
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<!--!introduction!--> The lower cell of the meridional overturning circulation (MOC) is sourced by dense Antarctic Bottom Water (AABW), which forms and sinks around Antarctica and subsequently fills the abyssal ocean. For the MOC to ‘overturn’, these dense waters must upwell through mixing with lighter waters above. Here, we investigate the processes underpinning such mixing, and the resulting water mass transformation, using an observationally forced, high-resolution numerical model of the Drake Passage in the Southern Ocean. In the Drake Passage, the mixing of dense AABW formed in the Weddell Sea with lighter deep waters transported from the Pacific Ocean by the Antarctic Circumpolar Current is catalysed by energetic flows impinging on rough topography. We find that multiple topographic interaction processes act to facilitate mixing of the two water masses, ultimately resulting in upwelling of waters with neutral density greater 28.19 kg m -3 , and downwelling of the lighter waters above. In ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ... |
format |
Conference Object |
author |
Baker, Lois Mashayek, Ali Naveira Garabato, Alberto |
spellingShingle |
Baker, Lois Mashayek, Ali Naveira Garabato, Alberto Enhanced upwelling of Antarctic Bottom Water by topographic interaction of water mass interfaces ... |
author_facet |
Baker, Lois Mashayek, Ali Naveira Garabato, Alberto |
author_sort |
Baker, Lois |
title |
Enhanced upwelling of Antarctic Bottom Water by topographic interaction of water mass interfaces ... |
title_short |
Enhanced upwelling of Antarctic Bottom Water by topographic interaction of water mass interfaces ... |
title_full |
Enhanced upwelling of Antarctic Bottom Water by topographic interaction of water mass interfaces ... |
title_fullStr |
Enhanced upwelling of Antarctic Bottom Water by topographic interaction of water mass interfaces ... |
title_full_unstemmed |
Enhanced upwelling of Antarctic Bottom Water by topographic interaction of water mass interfaces ... |
title_sort |
enhanced upwelling of antarctic bottom water by topographic interaction of water mass interfaces ... |
publisher |
GFZ German Research Centre for Geosciences |
publishDate |
2023 |
url |
https://dx.doi.org/10.57757/iugg23-1573 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018033 |
geographic |
Antarctic Southern Ocean The Antarctic Weddell Sea Drake Passage Pacific Weddell |
geographic_facet |
Antarctic Southern Ocean The Antarctic Weddell Sea Drake Passage Pacific Weddell |
genre |
Antarc* Antarctic Antarctica Drake Passage Southern Ocean Weddell Sea |
genre_facet |
Antarc* Antarctic Antarctica Drake Passage Southern Ocean Weddell Sea |
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/iugg23-1573 |
_version_ |
1772176936962883584 |