Vertical eddy energy fluxes in the North Atlantic subtropical and subpolar gyres

Eddy energy generation and energy fluxes are examined in a realistic eddy-resolving model of the North Atlantic. Over 80% of the wind energy input is found to be released by the generation of eddies through baroclinic instability. The eddy energy generation is located near the surface in the subtrop...

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Published in:Journal of Physical Oceanography
Main Authors: Zhai, X., Marshall, D.P.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2013
Subjects:
Online Access:https://ueaeprints.uea.ac.uk/id/eprint/43803/
https://doi.org/10.1175/JPO-D-12-021.1
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spelling ftuniveastangl:oai:ueaeprints.uea.ac.uk:43803 2023-05-15T17:28:09+02:00 Vertical eddy energy fluxes in the North Atlantic subtropical and subpolar gyres Zhai, X. Marshall, D.P. 2013-01-01 https://ueaeprints.uea.ac.uk/id/eprint/43803/ https://doi.org/10.1175/JPO-D-12-021.1 unknown Zhai, X. and Marshall, D.P. (2013) Vertical eddy energy fluxes in the North Atlantic subtropical and subpolar gyres. Journal of Physical Oceanography, 43 (1). pp. 95-103. ISSN 0022-3670 doi:10.1175/JPO-D-12-021.1 Article PeerReviewed 2013 ftuniveastangl https://doi.org/10.1175/JPO-D-12-021.1 2023-01-30T21:36:01Z Eddy energy generation and energy fluxes are examined in a realistic eddy-resolving model of the North Atlantic. Over 80% of the wind energy input is found to be released by the generation of eddies through baroclinic instability. The eddy energy generation is located near the surface in the subtropical gyre but deeper down in the subpolar gyre. To reconcile the mismatch between the depth of eddy energy production and the vertical structure of the horizontal dispersion of eddy energy, the vertical eddy energy flux is downward in the subtropical gyre and upward in the subpolar gyre. Article in Journal/Newspaper North Atlantic University of East Anglia: UEA Digital Repository Journal of Physical Oceanography 43 1 95 103
institution Open Polar
collection University of East Anglia: UEA Digital Repository
op_collection_id ftuniveastangl
language unknown
description Eddy energy generation and energy fluxes are examined in a realistic eddy-resolving model of the North Atlantic. Over 80% of the wind energy input is found to be released by the generation of eddies through baroclinic instability. The eddy energy generation is located near the surface in the subtropical gyre but deeper down in the subpolar gyre. To reconcile the mismatch between the depth of eddy energy production and the vertical structure of the horizontal dispersion of eddy energy, the vertical eddy energy flux is downward in the subtropical gyre and upward in the subpolar gyre.
format Article in Journal/Newspaper
author Zhai, X.
Marshall, D.P.
spellingShingle Zhai, X.
Marshall, D.P.
Vertical eddy energy fluxes in the North Atlantic subtropical and subpolar gyres
author_facet Zhai, X.
Marshall, D.P.
author_sort Zhai, X.
title Vertical eddy energy fluxes in the North Atlantic subtropical and subpolar gyres
title_short Vertical eddy energy fluxes in the North Atlantic subtropical and subpolar gyres
title_full Vertical eddy energy fluxes in the North Atlantic subtropical and subpolar gyres
title_fullStr Vertical eddy energy fluxes in the North Atlantic subtropical and subpolar gyres
title_full_unstemmed Vertical eddy energy fluxes in the North Atlantic subtropical and subpolar gyres
title_sort vertical eddy energy fluxes in the north atlantic subtropical and subpolar gyres
publishDate 2013
url https://ueaeprints.uea.ac.uk/id/eprint/43803/
https://doi.org/10.1175/JPO-D-12-021.1
genre North Atlantic
genre_facet North Atlantic
op_relation Zhai, X. and Marshall, D.P. (2013) Vertical eddy energy fluxes in the North Atlantic subtropical and subpolar gyres. Journal of Physical Oceanography, 43 (1). pp. 95-103. ISSN 0022-3670
doi:10.1175/JPO-D-12-021.1
op_doi https://doi.org/10.1175/JPO-D-12-021.1
container_title Journal of Physical Oceanography
container_volume 43
container_issue 1
container_start_page 95
op_container_end_page 103
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