Jets and Topography: Jet Transitions and the Impact on Transport in the Antarctic Circumpolar Current

The Southern Ocean's Antarctic Circumpolar Current (ACC) naturally lends itself to interpretations using a zonally averaged framework. Yet, navigation around steep and complicated bathymetric obstacles suggests that local dynamics may be far removed from those described by zonally symmetric mod...

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Published in:Journal of Physical Oceanography
Main Authors: Thompson, Andrew F., Sallée, Jean-Baptiste
Format: Article in Journal/Newspaper
Language:unknown
Published: American Meteorological Society 2012
Subjects:
Online Access:https://doi.org/10.1175/JPO-D-11-0135.1
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spelling ftcaltechauth:oai:authors.library.caltech.edu:apxt7-kbm57 2024-09-15T17:42:48+00:00 Jets and Topography: Jet Transitions and the Impact on Transport in the Antarctic Circumpolar Current Thompson, Andrew F. Sallée, Jean-Baptiste 2012-06 https://doi.org/10.1175/JPO-D-11-0135.1 unknown American Meteorological Society https://doi.org/10.1175/JPO-D-11-0135.1 oai:authors.library.caltech.edu:apxt7-kbm57 eprintid:32624 resolverid:CaltechAUTHORS:20120720-154002080 info:eu-repo/semantics/openAccess Other Journal of Physical Oceanography, 42(6), 956-972, (2012-06) info:eu-repo/semantics/article 2012 ftcaltechauth https://doi.org/10.1175/JPO-D-11-0135.1 2024-08-06T15:35:04Z The Southern Ocean's Antarctic Circumpolar Current (ACC) naturally lends itself to interpretations using a zonally averaged framework. Yet, navigation around steep and complicated bathymetric obstacles suggests that local dynamics may be far removed from those described by zonally symmetric models. In this study, both observational and numerical results indicate that zonal asymmetries, in the form of topography, impact global flow structure and transport properties. The conclusions are based on a suite of more than 1.5 million virtual drifter trajectories advected using a satellite altimetry–derived surface velocity field spanning 17 years. The focus is on sites of "cross front" transport as defined by movement across selected sea surface height contours that correspond to jets along most of the ACC. Cross-front exchange is localized in the lee of bathymetric features with more than 75% of crossing events occurring in regions corresponding to only 20% of the ACC's zonal extent. These observations motivate a series of numerical experiments using a two-layer quasigeostrophic model with simple, zonally asymmetric topography, which often produces transitions in the front structure along the channel. Significantly, regimes occur where the equilibrated number of coherent jets is a function of longitude and transport barriers are not periodic. Jet reorganization is carried out by eddy flux divergences acting to both accelerate and decelerate the mean flow of the jets. Eddy kinetic energy is amplified downstream of topography due to increased baroclinicity related to topographic steering. The combination of high eddy kinetic energy and recirculation features enhances particle exchange. These results stress the complications in developing consistent circumpolar definitions of the ACC fronts. © 2012 American Meteorological Society. Manuscript received 26 July 2011, in final form 13 December 2011. AFT was supported by a Natural Environment Research Council Advanced Research Fellowship (NE/H015760/1). We thank two ... Article in Journal/Newspaper Antarc* Antarctic Caltech Authors (California Institute of Technology) Journal of Physical Oceanography 42 6 956 972
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collection Caltech Authors (California Institute of Technology)
op_collection_id ftcaltechauth
language unknown
description The Southern Ocean's Antarctic Circumpolar Current (ACC) naturally lends itself to interpretations using a zonally averaged framework. Yet, navigation around steep and complicated bathymetric obstacles suggests that local dynamics may be far removed from those described by zonally symmetric models. In this study, both observational and numerical results indicate that zonal asymmetries, in the form of topography, impact global flow structure and transport properties. The conclusions are based on a suite of more than 1.5 million virtual drifter trajectories advected using a satellite altimetry–derived surface velocity field spanning 17 years. The focus is on sites of "cross front" transport as defined by movement across selected sea surface height contours that correspond to jets along most of the ACC. Cross-front exchange is localized in the lee of bathymetric features with more than 75% of crossing events occurring in regions corresponding to only 20% of the ACC's zonal extent. These observations motivate a series of numerical experiments using a two-layer quasigeostrophic model with simple, zonally asymmetric topography, which often produces transitions in the front structure along the channel. Significantly, regimes occur where the equilibrated number of coherent jets is a function of longitude and transport barriers are not periodic. Jet reorganization is carried out by eddy flux divergences acting to both accelerate and decelerate the mean flow of the jets. Eddy kinetic energy is amplified downstream of topography due to increased baroclinicity related to topographic steering. The combination of high eddy kinetic energy and recirculation features enhances particle exchange. These results stress the complications in developing consistent circumpolar definitions of the ACC fronts. © 2012 American Meteorological Society. Manuscript received 26 July 2011, in final form 13 December 2011. AFT was supported by a Natural Environment Research Council Advanced Research Fellowship (NE/H015760/1). We thank two ...
format Article in Journal/Newspaper
author Thompson, Andrew F.
Sallée, Jean-Baptiste
spellingShingle Thompson, Andrew F.
Sallée, Jean-Baptiste
Jets and Topography: Jet Transitions and the Impact on Transport in the Antarctic Circumpolar Current
author_facet Thompson, Andrew F.
Sallée, Jean-Baptiste
author_sort Thompson, Andrew F.
title Jets and Topography: Jet Transitions and the Impact on Transport in the Antarctic Circumpolar Current
title_short Jets and Topography: Jet Transitions and the Impact on Transport in the Antarctic Circumpolar Current
title_full Jets and Topography: Jet Transitions and the Impact on Transport in the Antarctic Circumpolar Current
title_fullStr Jets and Topography: Jet Transitions and the Impact on Transport in the Antarctic Circumpolar Current
title_full_unstemmed Jets and Topography: Jet Transitions and the Impact on Transport in the Antarctic Circumpolar Current
title_sort jets and topography: jet transitions and the impact on transport in the antarctic circumpolar current
publisher American Meteorological Society
publishDate 2012
url https://doi.org/10.1175/JPO-D-11-0135.1
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source Journal of Physical Oceanography, 42(6), 956-972, (2012-06)
op_relation https://doi.org/10.1175/JPO-D-11-0135.1
oai:authors.library.caltech.edu:apxt7-kbm57
eprintid:32624
resolverid:CaltechAUTHORS:20120720-154002080
op_rights info:eu-repo/semantics/openAccess
Other
op_doi https://doi.org/10.1175/JPO-D-11-0135.1
container_title Journal of Physical Oceanography
container_volume 42
container_issue 6
container_start_page 956
op_container_end_page 972
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