Modification of turbulent dissipation rates by a deep Southern Ocean eddy
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): 3450–3457, doi:10.1002/2015GL063216. The impact of a m...
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ftwhoas:oai:darchive.mblwhoilibrary.org:1912/7380 2023-05-15T18:24:48+02:00 Modification of turbulent dissipation rates by a deep Southern Ocean eddy Sheen, Katy L. Brearley, J. Alexander Naveira Garabato, Alberto C. Smeed, David A. St. Laurent, Louis C. Meredith, Michael P. Thurnherr, Andreas M. Waterman, Stephanie N. 2015-05-07 application/pdf https://hdl.handle.net/1912/7380 en_US eng John Wiley & Sons https://doi.org/10.1002/2015GL063216 Geophysical Research Letters 42 (2015): 3450–3457 https://hdl.handle.net/1912/7380 doi:10.1002/2015GL063216 Geophysical Research Letters 42 (2015): 3450–3457 doi:10.1002/2015GL063216 Mixing Eddy Turbulent dissipation Internal waves Southern Ocean Ray tracing Article 2015 ftwhoas https://doi.org/10.1002/2015GL063216 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): 3450–3457, doi:10.1002/2015GL063216. The impact of a mesoscale eddy on the magnitude and spatial distribution of diapycnal ocean mixing is investigated using a set of hydrographic and microstructure measurements collected in the Southern Ocean. These data sampled a baroclinic, middepth eddy formed during the disintegration of a deep boundary current. Turbulent dissipation is suppressed within the eddy but is elevated by up to an order of magnitude along the upper and lower eddy boundaries. A ray tracing approximation is employed as a heuristic device to elucidate how the internal wave field evolves in the ambient velocity and stratification conditions accompanying the eddy. These calculations are consistent with the observations, suggesting reflection of internal wave energy from the eddy center and enhanced breaking through critical layer processes along the eddy boundaries. These results have important implications for understanding where and how internal wave energy is dissipated in the presence of energetic deep geostrophic flows. Natural Environment Research Council (NERC). Grant Numbers: NE/E007058/1, NE/E005667/1; U.S. National Science Foundation. Grant Numbers: OCE-1231803, OCE-0927583, OCE-1030309; NERC 2015-11-07 Article in Journal/Newspaper Southern Ocean Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Southern Ocean Geophysical Research Letters 42 9 3450 3457 |
institution |
Open Polar |
collection |
Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) |
op_collection_id |
ftwhoas |
language |
English |
topic |
Mixing Eddy Turbulent dissipation Internal waves Southern Ocean Ray tracing |
spellingShingle |
Mixing Eddy Turbulent dissipation Internal waves Southern Ocean Ray tracing Sheen, Katy L. Brearley, J. Alexander Naveira Garabato, Alberto C. Smeed, David A. St. Laurent, Louis C. Meredith, Michael P. Thurnherr, Andreas M. Waterman, Stephanie N. Modification of turbulent dissipation rates by a deep Southern Ocean eddy |
topic_facet |
Mixing Eddy Turbulent dissipation Internal waves Southern Ocean Ray tracing |
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): 3450–3457, doi:10.1002/2015GL063216. The impact of a mesoscale eddy on the magnitude and spatial distribution of diapycnal ocean mixing is investigated using a set of hydrographic and microstructure measurements collected in the Southern Ocean. These data sampled a baroclinic, middepth eddy formed during the disintegration of a deep boundary current. Turbulent dissipation is suppressed within the eddy but is elevated by up to an order of magnitude along the upper and lower eddy boundaries. A ray tracing approximation is employed as a heuristic device to elucidate how the internal wave field evolves in the ambient velocity and stratification conditions accompanying the eddy. These calculations are consistent with the observations, suggesting reflection of internal wave energy from the eddy center and enhanced breaking through critical layer processes along the eddy boundaries. These results have important implications for understanding where and how internal wave energy is dissipated in the presence of energetic deep geostrophic flows. Natural Environment Research Council (NERC). Grant Numbers: NE/E007058/1, NE/E005667/1; U.S. National Science Foundation. Grant Numbers: OCE-1231803, OCE-0927583, OCE-1030309; NERC 2015-11-07 |
format |
Article in Journal/Newspaper |
author |
Sheen, Katy L. Brearley, J. Alexander Naveira Garabato, Alberto C. Smeed, David A. St. Laurent, Louis C. Meredith, Michael P. Thurnherr, Andreas M. Waterman, Stephanie N. |
author_facet |
Sheen, Katy L. Brearley, J. Alexander Naveira Garabato, Alberto C. Smeed, David A. St. Laurent, Louis C. Meredith, Michael P. Thurnherr, Andreas M. Waterman, Stephanie N. |
author_sort |
Sheen, Katy L. |
title |
Modification of turbulent dissipation rates by a deep Southern Ocean eddy |
title_short |
Modification of turbulent dissipation rates by a deep Southern Ocean eddy |
title_full |
Modification of turbulent dissipation rates by a deep Southern Ocean eddy |
title_fullStr |
Modification of turbulent dissipation rates by a deep Southern Ocean eddy |
title_full_unstemmed |
Modification of turbulent dissipation rates by a deep Southern Ocean eddy |
title_sort |
modification of turbulent dissipation rates by a deep southern ocean eddy |
publisher |
John Wiley & Sons |
publishDate |
2015 |
url |
https://hdl.handle.net/1912/7380 |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_source |
Geophysical Research Letters 42 (2015): 3450–3457 doi:10.1002/2015GL063216 |
op_relation |
https://doi.org/10.1002/2015GL063216 Geophysical Research Letters 42 (2015): 3450–3457 https://hdl.handle.net/1912/7380 doi:10.1002/2015GL063216 |
op_doi |
https://doi.org/10.1002/2015GL063216 |
container_title |
Geophysical Research Letters |
container_volume |
42 |
container_issue |
9 |
container_start_page |
3450 |
op_container_end_page |
3457 |
_version_ |
1766205730164047872 |