Can the ocean’s heat engine control horizontal circulation? Insights from the Caspian Sea.
We investigate the role of the ocean's heat engine in setting horizontal circulation using a numerical model of the Caspian Sea. The Caspian Sea can be seen as a virtual laboratory - a compromise between realistic global models which are hampered by long equilibration times and idealized basin...
Published in: | Geophysical Research Letters |
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American Geophysical Union
2017
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Online Access: | http://hdl.handle.net/10044/1/51030 https://doi.org/10.1002/2017GL075182 |
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ftimperialcol:oai:spiral.imperial.ac.uk:10044/1/51030 2023-05-15T18:25:27+02:00 Can the ocean’s heat engine control horizontal circulation? Insights from the Caspian Sea. Bruneau, N Zika, J Toumi, R 2017-09-15 http://hdl.handle.net/10044/1/51030 https://doi.org/10.1002/2017GL075182 unknown American Geophysical Union Geophysical Research Letters ©2017. The Authors. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. CC-BY 9900 9893 Science & Technology Physical Sciences Geosciences Multidisciplinary Geology SOUTHERN-OCEAN THERMOHALINE STRUCTURE SEASONAL VARIABILITY GENERAL-CIRCULATION MODEL CLIMATE FLUXES WATER TRANSPORT CLOSURE MD Multidisciplinary Meteorology & Atmospheric Sciences Journal Article 2017 ftimperialcol https://doi.org/10.1002/2017GL075182 2018-09-16T06:00:26Z We investigate the role of the ocean's heat engine in setting horizontal circulation using a numerical model of the Caspian Sea. The Caspian Sea can be seen as a virtual laboratory - a compromise between realistic global models which are hampered by long equilibration times and idealized basin geometry models which are not constrained by observations. We find that increases in vertical mixing drive stronger thermally direct overturning and consequent conversion of available potential to kinetic energy. Numerical solutions with water mass structures closest to observations overturn 0.02 − 0.04 x 106m3/s(Sv) representing the first estimate of Caspian Sea overturning. Our results also suggest that the overturning is thermally-forced increasing in intensity with increasing vertical diffusivity. Finally, stronger thermally direct overturning is associated with a stronger horizontal circulation in the Caspian Sea. This suggests the ocean's heat engine can strongly impact broader horizontal circulations in the ocean. Article in Journal/Newspaper Southern Ocean Imperial College London: Spiral Southern Ocean Geophysical Research Letters 44 19 9893 9900 |
institution |
Open Polar |
collection |
Imperial College London: Spiral |
op_collection_id |
ftimperialcol |
language |
unknown |
topic |
Science & Technology Physical Sciences Geosciences Multidisciplinary Geology SOUTHERN-OCEAN THERMOHALINE STRUCTURE SEASONAL VARIABILITY GENERAL-CIRCULATION MODEL CLIMATE FLUXES WATER TRANSPORT CLOSURE MD Multidisciplinary Meteorology & Atmospheric Sciences |
spellingShingle |
Science & Technology Physical Sciences Geosciences Multidisciplinary Geology SOUTHERN-OCEAN THERMOHALINE STRUCTURE SEASONAL VARIABILITY GENERAL-CIRCULATION MODEL CLIMATE FLUXES WATER TRANSPORT CLOSURE MD Multidisciplinary Meteorology & Atmospheric Sciences Bruneau, N Zika, J Toumi, R Can the ocean’s heat engine control horizontal circulation? Insights from the Caspian Sea. |
topic_facet |
Science & Technology Physical Sciences Geosciences Multidisciplinary Geology SOUTHERN-OCEAN THERMOHALINE STRUCTURE SEASONAL VARIABILITY GENERAL-CIRCULATION MODEL CLIMATE FLUXES WATER TRANSPORT CLOSURE MD Multidisciplinary Meteorology & Atmospheric Sciences |
description |
We investigate the role of the ocean's heat engine in setting horizontal circulation using a numerical model of the Caspian Sea. The Caspian Sea can be seen as a virtual laboratory - a compromise between realistic global models which are hampered by long equilibration times and idealized basin geometry models which are not constrained by observations. We find that increases in vertical mixing drive stronger thermally direct overturning and consequent conversion of available potential to kinetic energy. Numerical solutions with water mass structures closest to observations overturn 0.02 − 0.04 x 106m3/s(Sv) representing the first estimate of Caspian Sea overturning. Our results also suggest that the overturning is thermally-forced increasing in intensity with increasing vertical diffusivity. Finally, stronger thermally direct overturning is associated with a stronger horizontal circulation in the Caspian Sea. This suggests the ocean's heat engine can strongly impact broader horizontal circulations in the ocean. |
format |
Article in Journal/Newspaper |
author |
Bruneau, N Zika, J Toumi, R |
author_facet |
Bruneau, N Zika, J Toumi, R |
author_sort |
Bruneau, N |
title |
Can the ocean’s heat engine control horizontal circulation? Insights from the Caspian Sea. |
title_short |
Can the ocean’s heat engine control horizontal circulation? Insights from the Caspian Sea. |
title_full |
Can the ocean’s heat engine control horizontal circulation? Insights from the Caspian Sea. |
title_fullStr |
Can the ocean’s heat engine control horizontal circulation? Insights from the Caspian Sea. |
title_full_unstemmed |
Can the ocean’s heat engine control horizontal circulation? Insights from the Caspian Sea. |
title_sort |
can the ocean’s heat engine control horizontal circulation? insights from the caspian sea. |
publisher |
American Geophysical Union |
publishDate |
2017 |
url |
http://hdl.handle.net/10044/1/51030 https://doi.org/10.1002/2017GL075182 |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_source |
9900 9893 |
op_relation |
Geophysical Research Letters |
op_rights |
©2017. The Authors. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1002/2017GL075182 |
container_title |
Geophysical Research Letters |
container_volume |
44 |
container_issue |
19 |
container_start_page |
9893 |
op_container_end_page |
9900 |
_version_ |
1766206931476676608 |