Using Sea Level to Determine the Strength, Structure and Variability of the Cape Horn Current
The Cape Horn Current (CHC) is one of the components of the Antarctic Circumpolar Current system that enables it to fulfill its crucial role as a conduit between ocean basins. Despite this, to-date there have been very few measurements of CHC strength and none continuous in time or space. Here, we u...
Published in: | Geophysical Research Letters |
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2023
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Online Access: | https://hdl.handle.net/1983/391998c1-9985-47bc-92b5-1481f20bb291 https://research-information.bris.ac.uk/en/publications/391998c1-9985-47bc-92b5-1481f20bb291 https://doi.org/10.1029/2023GL105033 http://www.scopus.com/inward/record.url?scp=85175718866&partnerID=8YFLogxK |
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ftubristolcris:oai:research-information.bris.ac.uk:publications/391998c1-9985-47bc-92b5-1481f20bb291 2024-02-04T09:55:04+01:00 Using Sea Level to Determine the Strength, Structure and Variability of the Cape Horn Current Zheng, Qi Bingham, Rory Andrews, Oliver 2023-11-16 https://hdl.handle.net/1983/391998c1-9985-47bc-92b5-1481f20bb291 https://research-information.bris.ac.uk/en/publications/391998c1-9985-47bc-92b5-1481f20bb291 https://doi.org/10.1029/2023GL105033 http://www.scopus.com/inward/record.url?scp=85175718866&partnerID=8YFLogxK eng eng info:eu-repo/semantics/openAccess Zheng , Q , Bingham , R & Andrews , O 2023 , ' Using Sea Level to Determine the Strength, Structure and Variability of the Cape Horn Current ' , Geophysical Research Letters , vol. 50 , no. 21 , e2023GL105033 . https://doi.org/10.1029/2023GL105033 altimetry Cape Horn Current sea level volume transport article 2023 ftubristolcris https://doi.org/10.1029/2023GL105033 2024-01-11T23:51:02Z The Cape Horn Current (CHC) is one of the components of the Antarctic Circumpolar Current system that enables it to fulfill its crucial role as a conduit between ocean basins. Despite this, to-date there have been very few measurements of CHC strength and none continuous in time or space. Here, we use a combination of ocean models, one free-running and one data-assimilating, and satellite altimetry (1993–2021) to estimate the time-dependent strength of the CHC at 10 transects along its length. We find the time-mean CHC transport increases from 0.4 ± 0.5 Sv near 49°S to 5.3 ± 2.2 Sv at Cape Horn, with peak-to-peak interannual fluctuations of 0.8–3.4 Sv. Although, theoretically, increased run-off from a wasting Patagonian Ice-field would strengthen its flow, the CHC appears quite stable over the last 29 years, with little evidence of a coherent, long-term increase or decrease in the strength of the current. Article in Journal/Newspaper Antarc* Antarctic University of Bristol: Bristol Research Antarctic Cape Horn ENVELOPE(-135.021,-135.021,61.583,61.583) The Antarctic Geophysical Research Letters 50 21 |
institution |
Open Polar |
collection |
University of Bristol: Bristol Research |
op_collection_id |
ftubristolcris |
language |
English |
topic |
altimetry Cape Horn Current sea level volume transport |
spellingShingle |
altimetry Cape Horn Current sea level volume transport Zheng, Qi Bingham, Rory Andrews, Oliver Using Sea Level to Determine the Strength, Structure and Variability of the Cape Horn Current |
topic_facet |
altimetry Cape Horn Current sea level volume transport |
description |
The Cape Horn Current (CHC) is one of the components of the Antarctic Circumpolar Current system that enables it to fulfill its crucial role as a conduit between ocean basins. Despite this, to-date there have been very few measurements of CHC strength and none continuous in time or space. Here, we use a combination of ocean models, one free-running and one data-assimilating, and satellite altimetry (1993–2021) to estimate the time-dependent strength of the CHC at 10 transects along its length. We find the time-mean CHC transport increases from 0.4 ± 0.5 Sv near 49°S to 5.3 ± 2.2 Sv at Cape Horn, with peak-to-peak interannual fluctuations of 0.8–3.4 Sv. Although, theoretically, increased run-off from a wasting Patagonian Ice-field would strengthen its flow, the CHC appears quite stable over the last 29 years, with little evidence of a coherent, long-term increase or decrease in the strength of the current. |
format |
Article in Journal/Newspaper |
author |
Zheng, Qi Bingham, Rory Andrews, Oliver |
author_facet |
Zheng, Qi Bingham, Rory Andrews, Oliver |
author_sort |
Zheng, Qi |
title |
Using Sea Level to Determine the Strength, Structure and Variability of the Cape Horn Current |
title_short |
Using Sea Level to Determine the Strength, Structure and Variability of the Cape Horn Current |
title_full |
Using Sea Level to Determine the Strength, Structure and Variability of the Cape Horn Current |
title_fullStr |
Using Sea Level to Determine the Strength, Structure and Variability of the Cape Horn Current |
title_full_unstemmed |
Using Sea Level to Determine the Strength, Structure and Variability of the Cape Horn Current |
title_sort |
using sea level to determine the strength, structure and variability of the cape horn current |
publishDate |
2023 |
url |
https://hdl.handle.net/1983/391998c1-9985-47bc-92b5-1481f20bb291 https://research-information.bris.ac.uk/en/publications/391998c1-9985-47bc-92b5-1481f20bb291 https://doi.org/10.1029/2023GL105033 http://www.scopus.com/inward/record.url?scp=85175718866&partnerID=8YFLogxK |
long_lat |
ENVELOPE(-135.021,-135.021,61.583,61.583) |
geographic |
Antarctic Cape Horn The Antarctic |
geographic_facet |
Antarctic Cape Horn The Antarctic |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_source |
Zheng , Q , Bingham , R & Andrews , O 2023 , ' Using Sea Level to Determine the Strength, Structure and Variability of the Cape Horn Current ' , Geophysical Research Letters , vol. 50 , no. 21 , e2023GL105033 . https://doi.org/10.1029/2023GL105033 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1029/2023GL105033 |
container_title |
Geophysical Research Letters |
container_volume |
50 |
container_issue |
21 |
_version_ |
1789958932779761664 |