Submesoscale Rossby waves on the Antarctic circumpolar current. ...
The eastward-flowing Antarctic circumpolar current (ACC) plays a central role in the global ocean overturning circulation and facilitates the exchange of water between the ocean surface and interior. Submesoscale eddies and fronts with scales between 1 and 10 km are regularly observed in the upper o...
Main Authors: | , , , , , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Association for the Advancement of Science (AAAS)
2018
|
Subjects: | |
Online Access: | https://dx.doi.org/10.17863/cam.25694 https://www.repository.cam.ac.uk/handle/1810/278347 |
id |
ftdatacite:10.17863/cam.25694 |
---|---|
record_format |
openpolar |
spelling |
ftdatacite:10.17863/cam.25694 2024-02-27T08:35:06+00:00 Submesoscale Rossby waves on the Antarctic circumpolar current. ... Taylor, John R Bachman, Scott Stamper, Megan Hosegood, Phil Adams, Katherine Sallee, Jean-Baptiste Torres, Ricardo 2018 https://dx.doi.org/10.17863/cam.25694 https://www.repository.cam.ac.uk/handle/1810/278347 en eng American Association for the Advancement of Science (AAAS) open.access Creative Commons Attribution Non Commercial 4.0 International https://creativecommons.org/licenses/by-nc/4.0/legalcode cc-by-nc-4.0 http://purl.org/coar/access_right/c_abf2 0405 Oceanography article-journal ScholarlyArticle JournalArticle Article 2018 ftdatacite https://doi.org/10.17863/cam.25694 2024-02-01T14:57:51Z The eastward-flowing Antarctic circumpolar current (ACC) plays a central role in the global ocean overturning circulation and facilitates the exchange of water between the ocean surface and interior. Submesoscale eddies and fronts with scales between 1 and 10 km are regularly observed in the upper ocean and are associated with strong vertical circulations and enhanced stratification. Despite their importance in other locations, comparatively little is known about submesoscales in the Southern Ocean. We present results from new observations, models, and theories showing that submesoscales are qualitatively changed by the strong jet associated with the ACC in the Scotia Sea, east of Drake Passage. Growing submesoscale disturbances develop along a dense filament and are transformed into submesoscale Rossby waves, which propagate upstream relative to the eastward jet. Unlike their counterparts in slower currents, the submesoscale Rossby waves do not destroy the underlying frontal structure. The development of ... Article in Journal/Newspaper Antarc* Antarctic Drake Passage Scotia Sea Southern Ocean DataCite Metadata Store (German National Library of Science and Technology) Antarctic Drake Passage Scotia Sea Southern Ocean The Antarctic |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
0405 Oceanography |
spellingShingle |
0405 Oceanography Taylor, John R Bachman, Scott Stamper, Megan Hosegood, Phil Adams, Katherine Sallee, Jean-Baptiste Torres, Ricardo Submesoscale Rossby waves on the Antarctic circumpolar current. ... |
topic_facet |
0405 Oceanography |
description |
The eastward-flowing Antarctic circumpolar current (ACC) plays a central role in the global ocean overturning circulation and facilitates the exchange of water between the ocean surface and interior. Submesoscale eddies and fronts with scales between 1 and 10 km are regularly observed in the upper ocean and are associated with strong vertical circulations and enhanced stratification. Despite their importance in other locations, comparatively little is known about submesoscales in the Southern Ocean. We present results from new observations, models, and theories showing that submesoscales are qualitatively changed by the strong jet associated with the ACC in the Scotia Sea, east of Drake Passage. Growing submesoscale disturbances develop along a dense filament and are transformed into submesoscale Rossby waves, which propagate upstream relative to the eastward jet. Unlike their counterparts in slower currents, the submesoscale Rossby waves do not destroy the underlying frontal structure. The development of ... |
format |
Article in Journal/Newspaper |
author |
Taylor, John R Bachman, Scott Stamper, Megan Hosegood, Phil Adams, Katherine Sallee, Jean-Baptiste Torres, Ricardo |
author_facet |
Taylor, John R Bachman, Scott Stamper, Megan Hosegood, Phil Adams, Katherine Sallee, Jean-Baptiste Torres, Ricardo |
author_sort |
Taylor, John R |
title |
Submesoscale Rossby waves on the Antarctic circumpolar current. ... |
title_short |
Submesoscale Rossby waves on the Antarctic circumpolar current. ... |
title_full |
Submesoscale Rossby waves on the Antarctic circumpolar current. ... |
title_fullStr |
Submesoscale Rossby waves on the Antarctic circumpolar current. ... |
title_full_unstemmed |
Submesoscale Rossby waves on the Antarctic circumpolar current. ... |
title_sort |
submesoscale rossby waves on the antarctic circumpolar current. ... |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
2018 |
url |
https://dx.doi.org/10.17863/cam.25694 https://www.repository.cam.ac.uk/handle/1810/278347 |
geographic |
Antarctic Drake Passage Scotia Sea Southern Ocean The Antarctic |
geographic_facet |
Antarctic Drake Passage Scotia Sea Southern Ocean The Antarctic |
genre |
Antarc* Antarctic Drake Passage Scotia Sea Southern Ocean |
genre_facet |
Antarc* Antarctic Drake Passage Scotia Sea Southern Ocean |
op_rights |
open.access Creative Commons Attribution Non Commercial 4.0 International https://creativecommons.org/licenses/by-nc/4.0/legalcode cc-by-nc-4.0 http://purl.org/coar/access_right/c_abf2 |
op_doi |
https://doi.org/10.17863/cam.25694 |
_version_ |
1792041562498138112 |