Deglacial changes in flow and frontal structure through the Drake Passage ...
© 2017 Elsevier B.V. The oceanic gateways of the Drake Passage and the Agulhas Current are critical locations for the inflow of intermediate-depth water masses to the Atlantic, which contribute to the shallow return flow that balances the export of deep water from the North Atlantic. The thermohalin...
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ftdatacite:10.17863/cam.41687 2024-02-04T09:54:25+01:00 Deglacial changes in flow and frontal structure through the Drake Passage ... Roberts, J McCave, IN McClymont, EL Kender, S Hillenbrand, CD Matano, R Hodell, DA Peck, VL 2017 https://dx.doi.org/10.17863/cam.41687 https://www.repository.cam.ac.uk/handle/1810/294579 en eng Elsevier open.access Creative Commons Attribution Non Commercial No Derivatives 4.0 International https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode cc-by-nc-nd-4.0 http://purl.org/coar/access_right/c_abf2 cold water route sortable silt deglacial alkenones sub-Antarctic front Article ScholarlyArticle JournalArticle article-journal 2017 ftdatacite https://doi.org/10.17863/cam.41687 2024-01-05T09:28:50Z © 2017 Elsevier B.V. The oceanic gateways of the Drake Passage and the Agulhas Current are critical locations for the inflow of intermediate-depth water masses to the Atlantic, which contribute to the shallow return flow that balances the export of deep water from the North Atlantic. The thermohaline properties of northward flowing intermediate water are ultimately determined by the inflow of water through oceanic gateways. Here, we focus on the less well-studied “Cold Water Route” through the Drake Passage. We present millennially-resolved bottom current flow speed and sea surface temperature records downstream of the Drake Passage spanning the last 25,000 yr. We find that prior to 15 ka, bottom current flow speeds at sites in the Drake Passage region were dissimilar and there was a marked anti-phasing between sea surface temperatures at sites upstream and downstream of the Drake Passage. After 14 ka, we observe a remarkable convergence of flow speeds coupled with a sea surface temperature phase change at ... Article in Journal/Newspaper Antarc* Antarctic Drake Passage North Atlantic DataCite Metadata Store (German National Library of Science and Technology) Antarctic Drake Passage |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
cold water route sortable silt deglacial alkenones sub-Antarctic front |
spellingShingle |
cold water route sortable silt deglacial alkenones sub-Antarctic front Roberts, J McCave, IN McClymont, EL Kender, S Hillenbrand, CD Matano, R Hodell, DA Peck, VL Deglacial changes in flow and frontal structure through the Drake Passage ... |
topic_facet |
cold water route sortable silt deglacial alkenones sub-Antarctic front |
description |
© 2017 Elsevier B.V. The oceanic gateways of the Drake Passage and the Agulhas Current are critical locations for the inflow of intermediate-depth water masses to the Atlantic, which contribute to the shallow return flow that balances the export of deep water from the North Atlantic. The thermohaline properties of northward flowing intermediate water are ultimately determined by the inflow of water through oceanic gateways. Here, we focus on the less well-studied “Cold Water Route” through the Drake Passage. We present millennially-resolved bottom current flow speed and sea surface temperature records downstream of the Drake Passage spanning the last 25,000 yr. We find that prior to 15 ka, bottom current flow speeds at sites in the Drake Passage region were dissimilar and there was a marked anti-phasing between sea surface temperatures at sites upstream and downstream of the Drake Passage. After 14 ka, we observe a remarkable convergence of flow speeds coupled with a sea surface temperature phase change at ... |
format |
Article in Journal/Newspaper |
author |
Roberts, J McCave, IN McClymont, EL Kender, S Hillenbrand, CD Matano, R Hodell, DA Peck, VL |
author_facet |
Roberts, J McCave, IN McClymont, EL Kender, S Hillenbrand, CD Matano, R Hodell, DA Peck, VL |
author_sort |
Roberts, J |
title |
Deglacial changes in flow and frontal structure through the Drake Passage ... |
title_short |
Deglacial changes in flow and frontal structure through the Drake Passage ... |
title_full |
Deglacial changes in flow and frontal structure through the Drake Passage ... |
title_fullStr |
Deglacial changes in flow and frontal structure through the Drake Passage ... |
title_full_unstemmed |
Deglacial changes in flow and frontal structure through the Drake Passage ... |
title_sort |
deglacial changes in flow and frontal structure through the drake passage ... |
publisher |
Elsevier |
publishDate |
2017 |
url |
https://dx.doi.org/10.17863/cam.41687 https://www.repository.cam.ac.uk/handle/1810/294579 |
geographic |
Antarctic Drake Passage |
geographic_facet |
Antarctic Drake Passage |
genre |
Antarc* Antarctic Drake Passage North Atlantic |
genre_facet |
Antarc* Antarctic Drake Passage North Atlantic |
op_rights |
open.access Creative Commons Attribution Non Commercial No Derivatives 4.0 International https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode cc-by-nc-nd-4.0 http://purl.org/coar/access_right/c_abf2 |
op_doi |
https://doi.org/10.17863/cam.41687 |
_version_ |
1789973728059195392 |