Configuration of a Southern Ocean Storm Track

Diagnostics of ocean variability that reflect and influence local transport properties of heat and chemical species vary by an order of magnitude along the Southern Ocean’s Antarctic Circumpolar Current (ACC). Topographic “hotspots” are important regions of localized transport anomalies. This study...

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Published in:Journal of Physical Oceanography
Main Authors: Bischoff, Tobias, Thompson, Andrew F.
Format: Article in Journal/Newspaper
Language:English
Published: American Meteorological Society 2014
Subjects:
Online Access:https://authors.library.caltech.edu/53211/
https://authors.library.caltech.edu/53211/1/jpo-d-14-0062.1.pdf
https://resolver.caltech.edu/CaltechAUTHORS:20150106-125700649
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spelling ftcaltechauth:oai:authors.library.caltech.edu:53211 2023-05-15T13:57:16+02:00 Configuration of a Southern Ocean Storm Track Bischoff, Tobias Thompson, Andrew F. 2014-12 application/pdf https://authors.library.caltech.edu/53211/ https://authors.library.caltech.edu/53211/1/jpo-d-14-0062.1.pdf https://resolver.caltech.edu/CaltechAUTHORS:20150106-125700649 en eng American Meteorological Society https://authors.library.caltech.edu/53211/1/jpo-d-14-0062.1.pdf Bischoff, Tobias and Thompson, Andrew F. (2014) Configuration of a Southern Ocean Storm Track. Journal of Physical Oceanography, 44 (12). pp. 3072-3078. ISSN 0022-3670. doi:10.1175/JPO-D-14-0062.1. https://resolver.caltech.edu/CaltechAUTHORS:20150106-125700649 <https://resolver.caltech.edu/CaltechAUTHORS:20150106-125700649> other Article PeerReviewed 2014 ftcaltechauth https://doi.org/10.1175/JPO-D-14-0062.1 2021-11-11T19:01:51Z Diagnostics of ocean variability that reflect and influence local transport properties of heat and chemical species vary by an order of magnitude along the Southern Ocean’s Antarctic Circumpolar Current (ACC). Topographic “hotspots” are important regions of localized transport anomalies. This study uses a primitive equation channel model to investigate the structure of eddy kinetic energy (EKE), one measure of variability, in an oceanic regime. A storm-track approach emphasizes the importance of stationary eddies, which result from flow interactions with topography, on setting EKE distributions. The influence of these interactions extends far downstream of the topography and impacts EKE patterns through localized convergence and divergence of heat. Unlike for zonal averages, local contributions to the stationary fluxes from terms that integrate to zero in a zonal average are important. The simulations show a strong sensitivity of the zonal structure as well as the distribution and amplitude of stationary eddy fluxes to the surface wind forcing. By focusing on local, time-averaged stationary eddy fluxes, insight into the dynamical structure of the ACC can be gained that is concealed in the averaging procedure associated with traditional zonal or along-stream analyses. Article in Journal/Newspaper Antarc* Antarctic Southern Ocean Caltech Authors (California Institute of Technology) Antarctic Southern Ocean Journal of Physical Oceanography 44 12 3072 3078
institution Open Polar
collection Caltech Authors (California Institute of Technology)
op_collection_id ftcaltechauth
language English
description Diagnostics of ocean variability that reflect and influence local transport properties of heat and chemical species vary by an order of magnitude along the Southern Ocean’s Antarctic Circumpolar Current (ACC). Topographic “hotspots” are important regions of localized transport anomalies. This study uses a primitive equation channel model to investigate the structure of eddy kinetic energy (EKE), one measure of variability, in an oceanic regime. A storm-track approach emphasizes the importance of stationary eddies, which result from flow interactions with topography, on setting EKE distributions. The influence of these interactions extends far downstream of the topography and impacts EKE patterns through localized convergence and divergence of heat. Unlike for zonal averages, local contributions to the stationary fluxes from terms that integrate to zero in a zonal average are important. The simulations show a strong sensitivity of the zonal structure as well as the distribution and amplitude of stationary eddy fluxes to the surface wind forcing. By focusing on local, time-averaged stationary eddy fluxes, insight into the dynamical structure of the ACC can be gained that is concealed in the averaging procedure associated with traditional zonal or along-stream analyses.
format Article in Journal/Newspaper
author Bischoff, Tobias
Thompson, Andrew F.
spellingShingle Bischoff, Tobias
Thompson, Andrew F.
Configuration of a Southern Ocean Storm Track
author_facet Bischoff, Tobias
Thompson, Andrew F.
author_sort Bischoff, Tobias
title Configuration of a Southern Ocean Storm Track
title_short Configuration of a Southern Ocean Storm Track
title_full Configuration of a Southern Ocean Storm Track
title_fullStr Configuration of a Southern Ocean Storm Track
title_full_unstemmed Configuration of a Southern Ocean Storm Track
title_sort configuration of a southern ocean storm track
publisher American Meteorological Society
publishDate 2014
url https://authors.library.caltech.edu/53211/
https://authors.library.caltech.edu/53211/1/jpo-d-14-0062.1.pdf
https://resolver.caltech.edu/CaltechAUTHORS:20150106-125700649
geographic Antarctic
Southern Ocean
geographic_facet Antarctic
Southern Ocean
genre Antarc*
Antarctic
Southern Ocean
genre_facet Antarc*
Antarctic
Southern Ocean
op_relation https://authors.library.caltech.edu/53211/1/jpo-d-14-0062.1.pdf
Bischoff, Tobias and Thompson, Andrew F. (2014) Configuration of a Southern Ocean Storm Track. Journal of Physical Oceanography, 44 (12). pp. 3072-3078. ISSN 0022-3670. doi:10.1175/JPO-D-14-0062.1. https://resolver.caltech.edu/CaltechAUTHORS:20150106-125700649 <https://resolver.caltech.edu/CaltechAUTHORS:20150106-125700649>
op_rights other
op_doi https://doi.org/10.1175/JPO-D-14-0062.1
container_title Journal of Physical Oceanography
container_volume 44
container_issue 12
container_start_page 3072
op_container_end_page 3078
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