Surface eddy diffusivity for heat in a model of the northwest Atlantic Ocean

Eddies influence the surface beat budget both by modifying the surface heat flux and by the lateral transfer of heat within the surface mixed layer. It is shown that the presence of eddies modifies the surface heat flux in a model of the northwest Atlantic Ocean by more than 100 W m-2 over the Gulf...

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Published in:Geophysical Research Letters
Main Authors: Zhai, X, Greatbatch, R
Format: Article in Journal/Newspaper
Language:English
Published: 2016
Subjects:
Online Access:https://doi.org/10.1029/2006GL028712
https://ora.ox.ac.uk/objects/uuid:35136ff3-0ddf-4baf-af3f-c269eaa7a69f
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spelling ftuloxford:oai:ora.ox.ac.uk:uuid:35136ff3-0ddf-4baf-af3f-c269eaa7a69f 2023-05-15T17:45:30+02:00 Surface eddy diffusivity for heat in a model of the northwest Atlantic Ocean Zhai, X Greatbatch, R 2016-07-28 https://doi.org/10.1029/2006GL028712 https://ora.ox.ac.uk/objects/uuid:35136ff3-0ddf-4baf-af3f-c269eaa7a69f eng eng doi:10.1029/2006GL028712 https://ora.ox.ac.uk/objects/uuid:35136ff3-0ddf-4baf-af3f-c269eaa7a69f https://doi.org/10.1029/2006GL028712 info:eu-repo/semantics/embargoedAccess Journal article 2016 ftuloxford https://doi.org/10.1029/2006GL028712 2022-06-28T20:09:34Z Eddies influence the surface beat budget both by modifying the surface heat flux and by the lateral transfer of heat within the surface mixed layer. It is shown that the presence of eddies modifies the surface heat flux in a model of the northwest Atlantic Ocean by more than 100 W m-2 over the Gulf Stream system. The diffusive effect of eddies is then illustrated by comparing two model runs, in the second of which the surface heat flux acts only on large spatial scales and interaction with the mesoscale eddies is suppressed. This second run exhibits finer-scale structure and tighter thermal fronts than in the fully interactive run. Finally, we estimate the surface eddy diffusivity associated with surface thermal damping from the fully interactive run. The estimated diffusivity takes large values (more than 103 m2 s-1) south of the Gulf Stream and smaller values elsewhere. Copyright 2006 by the American Geophysical Union. Article in Journal/Newspaper Northwest Atlantic ORA - Oxford University Research Archive Geophysical Research Letters 33 24
institution Open Polar
collection ORA - Oxford University Research Archive
op_collection_id ftuloxford
language English
description Eddies influence the surface beat budget both by modifying the surface heat flux and by the lateral transfer of heat within the surface mixed layer. It is shown that the presence of eddies modifies the surface heat flux in a model of the northwest Atlantic Ocean by more than 100 W m-2 over the Gulf Stream system. The diffusive effect of eddies is then illustrated by comparing two model runs, in the second of which the surface heat flux acts only on large spatial scales and interaction with the mesoscale eddies is suppressed. This second run exhibits finer-scale structure and tighter thermal fronts than in the fully interactive run. Finally, we estimate the surface eddy diffusivity associated with surface thermal damping from the fully interactive run. The estimated diffusivity takes large values (more than 103 m2 s-1) south of the Gulf Stream and smaller values elsewhere. Copyright 2006 by the American Geophysical Union.
format Article in Journal/Newspaper
author Zhai, X
Greatbatch, R
spellingShingle Zhai, X
Greatbatch, R
Surface eddy diffusivity for heat in a model of the northwest Atlantic Ocean
author_facet Zhai, X
Greatbatch, R
author_sort Zhai, X
title Surface eddy diffusivity for heat in a model of the northwest Atlantic Ocean
title_short Surface eddy diffusivity for heat in a model of the northwest Atlantic Ocean
title_full Surface eddy diffusivity for heat in a model of the northwest Atlantic Ocean
title_fullStr Surface eddy diffusivity for heat in a model of the northwest Atlantic Ocean
title_full_unstemmed Surface eddy diffusivity for heat in a model of the northwest Atlantic Ocean
title_sort surface eddy diffusivity for heat in a model of the northwest atlantic ocean
publishDate 2016
url https://doi.org/10.1029/2006GL028712
https://ora.ox.ac.uk/objects/uuid:35136ff3-0ddf-4baf-af3f-c269eaa7a69f
genre Northwest Atlantic
genre_facet Northwest Atlantic
op_relation doi:10.1029/2006GL028712
https://ora.ox.ac.uk/objects/uuid:35136ff3-0ddf-4baf-af3f-c269eaa7a69f
https://doi.org/10.1029/2006GL028712
op_rights info:eu-repo/semantics/embargoedAccess
op_doi https://doi.org/10.1029/2006GL028712
container_title Geophysical Research Letters
container_volume 33
container_issue 24
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