Mapping the Antarctic Polar Front: weekly realizations from 2002 to 2014

We map the weekly position of the Antarctic Polar Front (PF) in the Southern Ocean over a 12-year period (2002–2014) using satellite sea surface temperature (SST) estimated from cloud-penetrating microwave radiometers. Our study advances previous efforts to map the PF using hydrographic and satellit...

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Main Authors: Freeman, Natalie Marie, Lovenduski, Nicole S.
Format: Text
Language:unknown
Published: CU Scholar 2016
Subjects:
Online Access:https://scholar.colorado.edu/atoc_facpapers/6
https://scholar.colorado.edu/cgi/viewcontent.cgi?article=1013&context=atoc_facpapers
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spelling ftunicolboulder:oai:scholar.colorado.edu:atoc_facpapers-1013 2023-05-15T13:49:40+02:00 Mapping the Antarctic Polar Front: weekly realizations from 2002 to 2014 Freeman, Natalie Marie Lovenduski, Nicole S. 2016-05-12T07:00:00Z application/pdf https://scholar.colorado.edu/atoc_facpapers/6 https://scholar.colorado.edu/cgi/viewcontent.cgi?article=1013&context=atoc_facpapers unknown CU Scholar https://scholar.colorado.edu/atoc_facpapers/6 https://scholar.colorado.edu/cgi/viewcontent.cgi?article=1013&context=atoc_facpapers Atmospheric & Oceanic Sciences Faculty Contributions text 2016 ftunicolboulder 2018-10-07T09:06:44Z We map the weekly position of the Antarctic Polar Front (PF) in the Southern Ocean over a 12-year period (2002–2014) using satellite sea surface temperature (SST) estimated from cloud-penetrating microwave radiometers. Our study advances previous efforts to map the PF using hydrographic and satellite data and provides a unique realization of the PF at weekly resolution across all longitudes (doi:10.1594/PANGAEA.855640). The mean path of the PF is asymmetric; its latitudinal position spans from 44 to 64° S along its circumpolar path. SST at the PF ranges from 0.6 to 6.9 °C, reflecting the large spread in latitudinal position. The average intensity of the front is 1.7 °C per 100 km, with intensity ranging from 1.4 to 2.3 °C per 100 km. Front intensity is significantly correlated with the depth of bottom topography, suggesting that the front intensifies over shallow bathymetry. Realizations of the PF are consistent with the corresponding surface expressions of the PF estimated using expendable bathythermograph data in the Drake Passage and Australian and African sectors. The climatological mean position of the PF is similar, though not identical, to previously published estimates. As the PF is a key indicator of physical circulation, surface nutrient concentration, and biogeography in the Southern Ocean, future studies of physical and biogeochemical oceanography in this region will benefit from the provided data set. Text Antarc* Antarctic Drake Passage Southern Ocean University of Colorado, Boulder: CU Scholar Antarctic Southern Ocean The Antarctic Drake Passage
institution Open Polar
collection University of Colorado, Boulder: CU Scholar
op_collection_id ftunicolboulder
language unknown
description We map the weekly position of the Antarctic Polar Front (PF) in the Southern Ocean over a 12-year period (2002–2014) using satellite sea surface temperature (SST) estimated from cloud-penetrating microwave radiometers. Our study advances previous efforts to map the PF using hydrographic and satellite data and provides a unique realization of the PF at weekly resolution across all longitudes (doi:10.1594/PANGAEA.855640). The mean path of the PF is asymmetric; its latitudinal position spans from 44 to 64° S along its circumpolar path. SST at the PF ranges from 0.6 to 6.9 °C, reflecting the large spread in latitudinal position. The average intensity of the front is 1.7 °C per 100 km, with intensity ranging from 1.4 to 2.3 °C per 100 km. Front intensity is significantly correlated with the depth of bottom topography, suggesting that the front intensifies over shallow bathymetry. Realizations of the PF are consistent with the corresponding surface expressions of the PF estimated using expendable bathythermograph data in the Drake Passage and Australian and African sectors. The climatological mean position of the PF is similar, though not identical, to previously published estimates. As the PF is a key indicator of physical circulation, surface nutrient concentration, and biogeography in the Southern Ocean, future studies of physical and biogeochemical oceanography in this region will benefit from the provided data set.
format Text
author Freeman, Natalie Marie
Lovenduski, Nicole S.
spellingShingle Freeman, Natalie Marie
Lovenduski, Nicole S.
Mapping the Antarctic Polar Front: weekly realizations from 2002 to 2014
author_facet Freeman, Natalie Marie
Lovenduski, Nicole S.
author_sort Freeman, Natalie Marie
title Mapping the Antarctic Polar Front: weekly realizations from 2002 to 2014
title_short Mapping the Antarctic Polar Front: weekly realizations from 2002 to 2014
title_full Mapping the Antarctic Polar Front: weekly realizations from 2002 to 2014
title_fullStr Mapping the Antarctic Polar Front: weekly realizations from 2002 to 2014
title_full_unstemmed Mapping the Antarctic Polar Front: weekly realizations from 2002 to 2014
title_sort mapping the antarctic polar front: weekly realizations from 2002 to 2014
publisher CU Scholar
publishDate 2016
url https://scholar.colorado.edu/atoc_facpapers/6
https://scholar.colorado.edu/cgi/viewcontent.cgi?article=1013&context=atoc_facpapers
geographic Antarctic
Southern Ocean
The Antarctic
Drake Passage
geographic_facet Antarctic
Southern Ocean
The Antarctic
Drake Passage
genre Antarc*
Antarctic
Drake Passage
Southern Ocean
genre_facet Antarc*
Antarctic
Drake Passage
Southern Ocean
op_source Atmospheric & Oceanic Sciences Faculty Contributions
op_relation https://scholar.colorado.edu/atoc_facpapers/6
https://scholar.colorado.edu/cgi/viewcontent.cgi?article=1013&context=atoc_facpapers
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