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 basins r...

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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://authors.library.caltech.edu/81887/
https://resolver.caltech.edu/CaltechAUTHORS:20170927-152756537
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spelling ftcaltechauth:oai:authors.library.caltech.edu:81887 2023-05-15T13:55:46+02:00 Physical-Biogeochemical Coupling in the Southern Ocean Thompson, Andrew F. Cassar, Nicolas 2015-10-09 https://authors.library.caltech.edu/81887/ https://resolver.caltech.edu/CaltechAUTHORS:20170927-152756537 unknown Wiley Thompson, Andrew F. and Cassar, Nicolas (2015) Physical-Biogeochemical Coupling in the Southern Ocean. Eos, 96 . ISSN 2324-9250. doi:10.1029/2015EO036829. https://resolver.caltech.edu/CaltechAUTHORS:20170927-152756537 <https://resolver.caltech.edu/CaltechAUTHORS:20170927-152756537> Article PeerReviewed 2015 ftcaltechauth https://doi.org/10.1029/2015EO036829 2021-11-18T18:43:51Z 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. 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.
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://authors.library.caltech.edu/81887/
https://resolver.caltech.edu/CaltechAUTHORS:20170927-152756537
geographic Southern Ocean
geographic_facet Southern Ocean
genre Antarc*
Antarctica
Southern Ocean
genre_facet Antarc*
Antarctica
Southern Ocean
op_relation Thompson, Andrew F. and Cassar, Nicolas (2015) Physical-Biogeochemical Coupling in the Southern Ocean. Eos, 96 . ISSN 2324-9250. doi:10.1029/2015EO036829. https://resolver.caltech.edu/CaltechAUTHORS:20170927-152756537 <https://resolver.caltech.edu/CaltechAUTHORS:20170927-152756537>
op_doi https://doi.org/10.1029/2015EO036829
container_title Eos
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