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

Eddies influence the surface heat 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, Xiaoming, Greatbatch, Richard J.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2006
Subjects:
Online Access:https://ueaeprints.uea.ac.uk/id/eprint/43792/
https://doi.org/10.1029/2006GL028712
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spelling ftuniveastangl:oai:ueaeprints.uea.ac.uk:43792 2023-05-15T17:45:29+02:00 Surface eddy diffusivity for heat in a model of the northwest Atlantic Ocean Zhai, Xiaoming Greatbatch, Richard J. 2006-12 https://ueaeprints.uea.ac.uk/id/eprint/43792/ https://doi.org/10.1029/2006GL028712 unknown Zhai, Xiaoming and Greatbatch, Richard J. (2006) Surface eddy diffusivity for heat in a model of the northwest Atlantic Ocean. Geophysical Research Letters, 33 (24). ISSN 0094-8276 doi:10.1029/2006GL028712 Article PeerReviewed 2006 ftuniveastangl https://doi.org/10.1029/2006GL028712 2023-01-30T21:36:01Z Eddies influence the surface heat 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. Article in Journal/Newspaper Northwest Atlantic University of East Anglia: UEA Digital Repository Geophysical Research Letters 33 24
institution Open Polar
collection University of East Anglia: UEA Digital Repository
op_collection_id ftuniveastangl
language unknown
description Eddies influence the surface heat 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.
format Article in Journal/Newspaper
author Zhai, Xiaoming
Greatbatch, Richard J.
spellingShingle Zhai, Xiaoming
Greatbatch, Richard J.
Surface eddy diffusivity for heat in a model of the northwest Atlantic Ocean
author_facet Zhai, Xiaoming
Greatbatch, Richard J.
author_sort Zhai, Xiaoming
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 2006
url https://ueaeprints.uea.ac.uk/id/eprint/43792/
https://doi.org/10.1029/2006GL028712
genre Northwest Atlantic
genre_facet Northwest Atlantic
op_relation Zhai, Xiaoming and Greatbatch, Richard J. (2006) Surface eddy diffusivity for heat in a model of the northwest Atlantic Ocean. Geophysical Research Letters, 33 (24). ISSN 0094-8276
doi:10.1029/2006GL028712
op_doi https://doi.org/10.1029/2006GL028712
container_title Geophysical Research Letters
container_volume 33
container_issue 24
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