Rapid injection of near-inertial shear into the stratified upper ocean at an Antarctic Circumpolar Current front
Author Posting. © American Geophysical Union, 2015. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 42 (2015): 3431–3441, doi:10.1002/2015GL063494. The impact on the...
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Online Access: | https://hdl.handle.net/1912/7371 |
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ftwhoas:oai:darchive.mblwhoilibrary.org:1912/7371 2023-05-15T13:53:15+02:00 Rapid injection of near-inertial shear into the stratified upper ocean at an Antarctic Circumpolar Current front Forryan, Alexander Naveira Garabato, Alberto C. Polzin, Kurt L. Waterman, Stephanie N. 2015-05-07 application/pdf https://hdl.handle.net/1912/7371 en_US eng John Wiley & Sons https://doi.org/10.1002/2015GL063494 Geophysical Research Letters 42 (2015): 3431–3441 https://hdl.handle.net/1912/7371 doi:10.1002/2015GL063494 Geophysical Research Letters 42 (2015): 3431–3441 doi:10.1002/2015GL063494 Upper ocean Restratification Near-inertial shear Article 2015 ftwhoas https://doi.org/10.1002/2015GL063494 2022-05-28T22:59:21Z Author Posting. © American Geophysical Union, 2015. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 42 (2015): 3431–3441, doi:10.1002/2015GL063494. The impact on the upper ocean of the passage of a short, intense storm over a Southern Ocean site, in proximity to an Antarctic Circumpolar Current front, is characterized. The storm causes a wind-induced deepening of the mixed layer and generates an inertial current. Immediate poststorm observations indicate a mixed layer extending to approximately 50 m depth. Subsequent measurements show the upper ocean to have restratified, injecting near-inertial shear in stratified waters within 1 day of the storm's passage. This time scale for the development of near-inertial shear is 1 order of magnitude shorter than that predicted by the β dispersion paradigm. The observed rapid changes in upper ocean stratification point to the existence of an as yet undocumented, efficient mechanism for injection of near-inertial shear into the stratified ocean that is in turn associated with enhanced turbulence and mixing. The SOFine project is funded by the UK Natural Environmental Research Council (NERC) (grant NE/G001510/1). 2015-11-07 Article in Journal/Newspaper Antarc* Antarctic Southern Ocean Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Antarctic Southern Ocean Geophysical Research Letters 42 9 3431 3441 |
institution |
Open Polar |
collection |
Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) |
op_collection_id |
ftwhoas |
language |
English |
topic |
Upper ocean Restratification Near-inertial shear |
spellingShingle |
Upper ocean Restratification Near-inertial shear Forryan, Alexander Naveira Garabato, Alberto C. Polzin, Kurt L. Waterman, Stephanie N. Rapid injection of near-inertial shear into the stratified upper ocean at an Antarctic Circumpolar Current front |
topic_facet |
Upper ocean Restratification Near-inertial shear |
description |
Author Posting. © American Geophysical Union, 2015. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 42 (2015): 3431–3441, doi:10.1002/2015GL063494. The impact on the upper ocean of the passage of a short, intense storm over a Southern Ocean site, in proximity to an Antarctic Circumpolar Current front, is characterized. The storm causes a wind-induced deepening of the mixed layer and generates an inertial current. Immediate poststorm observations indicate a mixed layer extending to approximately 50 m depth. Subsequent measurements show the upper ocean to have restratified, injecting near-inertial shear in stratified waters within 1 day of the storm's passage. This time scale for the development of near-inertial shear is 1 order of magnitude shorter than that predicted by the β dispersion paradigm. The observed rapid changes in upper ocean stratification point to the existence of an as yet undocumented, efficient mechanism for injection of near-inertial shear into the stratified ocean that is in turn associated with enhanced turbulence and mixing. The SOFine project is funded by the UK Natural Environmental Research Council (NERC) (grant NE/G001510/1). 2015-11-07 |
format |
Article in Journal/Newspaper |
author |
Forryan, Alexander Naveira Garabato, Alberto C. Polzin, Kurt L. Waterman, Stephanie N. |
author_facet |
Forryan, Alexander Naveira Garabato, Alberto C. Polzin, Kurt L. Waterman, Stephanie N. |
author_sort |
Forryan, Alexander |
title |
Rapid injection of near-inertial shear into the stratified upper ocean at an Antarctic Circumpolar Current front |
title_short |
Rapid injection of near-inertial shear into the stratified upper ocean at an Antarctic Circumpolar Current front |
title_full |
Rapid injection of near-inertial shear into the stratified upper ocean at an Antarctic Circumpolar Current front |
title_fullStr |
Rapid injection of near-inertial shear into the stratified upper ocean at an Antarctic Circumpolar Current front |
title_full_unstemmed |
Rapid injection of near-inertial shear into the stratified upper ocean at an Antarctic Circumpolar Current front |
title_sort |
rapid injection of near-inertial shear into the stratified upper ocean at an antarctic circumpolar current front |
publisher |
John Wiley & Sons |
publishDate |
2015 |
url |
https://hdl.handle.net/1912/7371 |
geographic |
Antarctic Southern Ocean |
geographic_facet |
Antarctic Southern Ocean |
genre |
Antarc* Antarctic Southern Ocean |
genre_facet |
Antarc* Antarctic Southern Ocean |
op_source |
Geophysical Research Letters 42 (2015): 3431–3441 doi:10.1002/2015GL063494 |
op_relation |
https://doi.org/10.1002/2015GL063494 Geophysical Research Letters 42 (2015): 3431–3441 https://hdl.handle.net/1912/7371 doi:10.1002/2015GL063494 |
op_doi |
https://doi.org/10.1002/2015GL063494 |
container_title |
Geophysical Research Letters |
container_volume |
42 |
container_issue |
9 |
container_start_page |
3431 |
op_container_end_page |
3441 |
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1766258256695525376 |