Wind work in a model of the northwest Atlantic Ocean

The work done by the wind over the northwest Atlantic Ocean is examined using a realistic high-resolution ocean model driven by synoptic wind forcing. Two model runs are conducted with the difference only in the way the wind stress is calculated. Our results show that the effect of including ocean s...

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Published in:Geophysical Research Letters
Main Authors: Zhai, Xiaoming, Greatbatch, Richard J.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2007
Subjects:
Online Access:https://ueaeprints.uea.ac.uk/id/eprint/43793/
https://doi.org/10.1029/2006GL028907
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spelling ftuniveastangl:oai:ueaeprints.uea.ac.uk:43793 2023-05-15T17:45:29+02:00 Wind work in a model of the northwest Atlantic Ocean Zhai, Xiaoming Greatbatch, Richard J. 2007-02 https://ueaeprints.uea.ac.uk/id/eprint/43793/ https://doi.org/10.1029/2006GL028907 unknown Zhai, Xiaoming and Greatbatch, Richard J. (2007) Wind work in a model of the northwest Atlantic Ocean. Geophysical Research Letters, 34 (4). ISSN 0094-8276 doi:10.1029/2006GL028907 Article PeerReviewed 2007 ftuniveastangl https://doi.org/10.1029/2006GL028907 2023-01-30T21:36:01Z The work done by the wind over the northwest Atlantic Ocean is examined using a realistic high-resolution ocean model driven by synoptic wind forcing. Two model runs are conducted with the difference only in the way the wind stress is calculated. Our results show that the effect of including ocean surface currents in the wind stress formulation is to reduce the total wind work integrated over the model domain by about 17%. The reduction is caused by a sink term in the wind work calculation associated with the presence of ocean currents. In addition, the modelled eddy kinetic energy decreases by about 10%, in response to direct mechanical damping by the surface stress. A simple scaling argument shows that the latter can be expected to be more important than bottom friction in the energy budget. Article in Journal/Newspaper Northwest Atlantic University of East Anglia: UEA Digital Repository Geophysical Research Letters 34 4
institution Open Polar
collection University of East Anglia: UEA Digital Repository
op_collection_id ftuniveastangl
language unknown
description The work done by the wind over the northwest Atlantic Ocean is examined using a realistic high-resolution ocean model driven by synoptic wind forcing. Two model runs are conducted with the difference only in the way the wind stress is calculated. Our results show that the effect of including ocean surface currents in the wind stress formulation is to reduce the total wind work integrated over the model domain by about 17%. The reduction is caused by a sink term in the wind work calculation associated with the presence of ocean currents. In addition, the modelled eddy kinetic energy decreases by about 10%, in response to direct mechanical damping by the surface stress. A simple scaling argument shows that the latter can be expected to be more important than bottom friction in the energy budget.
format Article in Journal/Newspaper
author Zhai, Xiaoming
Greatbatch, Richard J.
spellingShingle Zhai, Xiaoming
Greatbatch, Richard J.
Wind work in a model of the northwest Atlantic Ocean
author_facet Zhai, Xiaoming
Greatbatch, Richard J.
author_sort Zhai, Xiaoming
title Wind work in a model of the northwest Atlantic Ocean
title_short Wind work in a model of the northwest Atlantic Ocean
title_full Wind work in a model of the northwest Atlantic Ocean
title_fullStr Wind work in a model of the northwest Atlantic Ocean
title_full_unstemmed Wind work in a model of the northwest Atlantic Ocean
title_sort wind work in a model of the northwest atlantic ocean
publishDate 2007
url https://ueaeprints.uea.ac.uk/id/eprint/43793/
https://doi.org/10.1029/2006GL028907
genre Northwest Atlantic
genre_facet Northwest Atlantic
op_relation Zhai, Xiaoming and Greatbatch, Richard J. (2007) Wind work in a model of the northwest Atlantic Ocean. Geophysical Research Letters, 34 (4). ISSN 0094-8276
doi:10.1029/2006GL028907
op_doi https://doi.org/10.1029/2006GL028907
container_title Geophysical Research Letters
container_volume 34
container_issue 4
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