Physical-Biogeochemical Coupling in the Southern Ocean

Over the past 15 years, physical and biogeochemical studies have established that the Southern Ocean, the region surrounding Antarctica, plays a disproportionately large role in modulating Earth's climate. Dense water masses that reside near the ocean bottom throughout mid- and low-latitude bas...

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Published in:Eos
Main Authors: Thompson, Andrew F., Cassar, Nicolas
Format: Article in Journal/Newspaper
Language:unknown
Published: Wiley 2015
Subjects:
Online Access:https://doi.org/10.1029/2015EO036829
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spelling ftcaltechauth:oai:authors.library.caltech.edu:4yq3c-8b393 2024-06-23T07:46:00+00:00 Physical-Biogeochemical Coupling in the Southern Ocean Thompson, Andrew F. Cassar, Nicolas 2015-10-09 https://doi.org/10.1029/2015EO036829 unknown Wiley https://doi.org/10.1029/2015EO036829 oai:authors.library.caltech.edu:4yq3c-8b393 eprintid:81887 resolverid:CaltechAUTHORS:20170927-152756537 info:eu-repo/semantics/closedAccess Other Eos, 96, (2015-10-09) Southern Ocean Dynamics and Biogeochemistry Workshop, Pasadena, CA, 2-5 February 2015 info:eu-repo/semantics/article 2015 ftcaltechauth https://doi.org/10.1029/2015EO036829 2024-06-12T06:34:27Z Over the past 15 years, physical and biogeochemical studies have established that the Southern Ocean, the region surrounding Antarctica, plays a disproportionately large role in modulating Earth's climate. Dense water masses that reside near the ocean bottom throughout mid- and low-latitude basins reach the surface in the Southern Ocean through a combination of wind- and eddy-induced transport. These waters are exposed to heat, freshwater fluxes, and atmospheric gases, which ventilate the deep-ocean reservoirs of heat and carbon. © 2015. The authors. CC BY-NC 3.0. Article in Journal/Newspaper Antarc* Antarctica Southern Ocean Caltech Authors (California Institute of Technology) Southern Ocean Eos
institution Open Polar
collection Caltech Authors (California Institute of Technology)
op_collection_id ftcaltechauth
language unknown
description Over the past 15 years, physical and biogeochemical studies have established that the Southern Ocean, the region surrounding Antarctica, plays a disproportionately large role in modulating Earth's climate. Dense water masses that reside near the ocean bottom throughout mid- and low-latitude basins reach the surface in the Southern Ocean through a combination of wind- and eddy-induced transport. These waters are exposed to heat, freshwater fluxes, and atmospheric gases, which ventilate the deep-ocean reservoirs of heat and carbon. © 2015. The authors. CC BY-NC 3.0.
format Article in Journal/Newspaper
author Thompson, Andrew F.
Cassar, Nicolas
spellingShingle Thompson, Andrew F.
Cassar, Nicolas
Physical-Biogeochemical Coupling in the Southern Ocean
author_facet Thompson, Andrew F.
Cassar, Nicolas
author_sort Thompson, Andrew F.
title Physical-Biogeochemical Coupling in the Southern Ocean
title_short Physical-Biogeochemical Coupling in the Southern Ocean
title_full Physical-Biogeochemical Coupling in the Southern Ocean
title_fullStr Physical-Biogeochemical Coupling in the Southern Ocean
title_full_unstemmed Physical-Biogeochemical Coupling in the Southern Ocean
title_sort physical-biogeochemical coupling in the southern ocean
publisher Wiley
publishDate 2015
url https://doi.org/10.1029/2015EO036829
geographic Southern Ocean
geographic_facet Southern Ocean
genre Antarc*
Antarctica
Southern Ocean
genre_facet Antarc*
Antarctica
Southern Ocean
op_source Eos, 96, (2015-10-09)
Southern Ocean Dynamics and Biogeochemistry Workshop, Pasadena, CA, 2-5 February 2015
op_relation https://doi.org/10.1029/2015EO036829
oai:authors.library.caltech.edu:4yq3c-8b393
eprintid:81887
resolverid:CaltechAUTHORS:20170927-152756537
op_rights info:eu-repo/semantics/closedAccess
Other
op_doi https://doi.org/10.1029/2015EO036829
container_title Eos
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