Advection of baroclinic eddies by depth mean flow

Observed zonal propagation speeds of nonlinear eddies, derived using an eddy tracking algorithm, are compared with the classical long Rossby wave speed, Doppler shifted by just the depth mean velocity, the latter obtained from annual mean hydrography and an ocean atlas. Despite neglecting any Dopple...

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Published in:Geophysical Research Letters
Main Authors: Klocker, A, Marshall, D
Format: Article in Journal/Newspaper
Language:English
Published: Blackwell Publishing Ltd 2016
Subjects:
Online Access:https://doi.org/10.1002/2014GL060001
https://ora.ox.ac.uk/objects/uuid:f6ce659c-4ee4-44f8-b811-62d142144b22
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spelling ftuloxford:oai:ora.ox.ac.uk:uuid:f6ce659c-4ee4-44f8-b811-62d142144b22 2023-05-15T13:56:24+02:00 Advection of baroclinic eddies by depth mean flow Klocker, A Marshall, D 2016-07-29 https://doi.org/10.1002/2014GL060001 https://ora.ox.ac.uk/objects/uuid:f6ce659c-4ee4-44f8-b811-62d142144b22 eng eng Blackwell Publishing Ltd doi:10.1002/2014GL060001 https://ora.ox.ac.uk/objects/uuid:f6ce659c-4ee4-44f8-b811-62d142144b22 https://doi.org/10.1002/2014GL060001 info:eu-repo/semantics/embargoedAccess Journal article 2016 ftuloxford https://doi.org/10.1002/2014GL060001 2022-06-28T20:28:18Z Observed zonal propagation speeds of nonlinear eddies, derived using an eddy tracking algorithm, are compared with the classical long Rossby wave speed, Doppler shifted by just the depth mean velocity, the latter obtained from annual mean hydrography and an ocean atlas. Despite neglecting any Doppler shift from baroclinic background flows, the correspondence between observed eddy propagation speeds and theoretical long Rossby wave phase speeds is improved in the Antarctic Circumpolar Current region, where both show eastward propagation at speeds of 1-3cms-1, although the observed eastward eddy propagation speeds are systematically lower than the predicted Rossby wave phase speeds. © 2014. American Geophysical Union. All Rights Reserved. Article in Journal/Newspaper Antarc* Antarctic ORA - Oxford University Research Archive Antarctic The Antarctic Geophysical Research Letters 41 10 3517 3521
institution Open Polar
collection ORA - Oxford University Research Archive
op_collection_id ftuloxford
language English
description Observed zonal propagation speeds of nonlinear eddies, derived using an eddy tracking algorithm, are compared with the classical long Rossby wave speed, Doppler shifted by just the depth mean velocity, the latter obtained from annual mean hydrography and an ocean atlas. Despite neglecting any Doppler shift from baroclinic background flows, the correspondence between observed eddy propagation speeds and theoretical long Rossby wave phase speeds is improved in the Antarctic Circumpolar Current region, where both show eastward propagation at speeds of 1-3cms-1, although the observed eastward eddy propagation speeds are systematically lower than the predicted Rossby wave phase speeds. © 2014. American Geophysical Union. All Rights Reserved.
format Article in Journal/Newspaper
author Klocker, A
Marshall, D
spellingShingle Klocker, A
Marshall, D
Advection of baroclinic eddies by depth mean flow
author_facet Klocker, A
Marshall, D
author_sort Klocker, A
title Advection of baroclinic eddies by depth mean flow
title_short Advection of baroclinic eddies by depth mean flow
title_full Advection of baroclinic eddies by depth mean flow
title_fullStr Advection of baroclinic eddies by depth mean flow
title_full_unstemmed Advection of baroclinic eddies by depth mean flow
title_sort advection of baroclinic eddies by depth mean flow
publisher Blackwell Publishing Ltd
publishDate 2016
url https://doi.org/10.1002/2014GL060001
https://ora.ox.ac.uk/objects/uuid:f6ce659c-4ee4-44f8-b811-62d142144b22
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_relation doi:10.1002/2014GL060001
https://ora.ox.ac.uk/objects/uuid:f6ce659c-4ee4-44f8-b811-62d142144b22
https://doi.org/10.1002/2014GL060001
op_rights info:eu-repo/semantics/embargoedAccess
op_doi https://doi.org/10.1002/2014GL060001
container_title Geophysical Research Letters
container_volume 41
container_issue 10
container_start_page 3517
op_container_end_page 3521
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