Sea-ice-driven shallow overturning

Circumpolar upwelling circulation near the Antarctic has mainly been attributed to winds. An analysis ofwater-mass transformation shows that the dominant driver is instead the formation of sea ice near Antarctica andits melt offshore.

Bibliographic Details
Published in:Nature Geoscience
Main Authors: Bindoff, NL, Hobbs, WR
Format: Text
Language:English
Published: Nature Publishing Group 2016
Subjects:
Online Access:https://doi.org/10.1038/ngeo2766
http://ecite.utas.edu.au/109702
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spelling ftunivtasecite:oai:ecite.utas.edu.au:109702 2023-05-15T14:03:26+02:00 Sea-ice-driven shallow overturning Bindoff, NL Hobbs, WR 2016 application/pdf https://doi.org/10.1038/ngeo2766 http://ecite.utas.edu.au/109702 en eng Nature Publishing Group http://ecite.utas.edu.au/109702/1/ngeo2766.pdf http://dx.doi.org/10.1038/ngeo2766 Bindoff, NL and Hobbs, WR, Sea-ice-driven shallow overturning, Nature Geoscience, 9, (8) pp. 569-570. ISSN 1752-0894 (2016) [Non Refereed Article] http://ecite.utas.edu.au/109702 Earth Sciences Oceanography Physical Oceanography Non Refereed Article NonPeerReviewed 2016 ftunivtasecite https://doi.org/10.1038/ngeo2766 2019-12-13T22:10:19Z Circumpolar upwelling circulation near the Antarctic has mainly been attributed to winds. An analysis ofwater-mass transformation shows that the dominant driver is instead the formation of sea ice near Antarctica andits melt offshore. Text Antarc* Antarctic Antarctica Sea ice eCite UTAS (University of Tasmania) Antarctic The Antarctic Nature Geoscience 9 8 569 570
institution Open Polar
collection eCite UTAS (University of Tasmania)
op_collection_id ftunivtasecite
language English
topic Earth Sciences
Oceanography
Physical Oceanography
spellingShingle Earth Sciences
Oceanography
Physical Oceanography
Bindoff, NL
Hobbs, WR
Sea-ice-driven shallow overturning
topic_facet Earth Sciences
Oceanography
Physical Oceanography
description Circumpolar upwelling circulation near the Antarctic has mainly been attributed to winds. An analysis ofwater-mass transformation shows that the dominant driver is instead the formation of sea ice near Antarctica andits melt offshore.
format Text
author Bindoff, NL
Hobbs, WR
author_facet Bindoff, NL
Hobbs, WR
author_sort Bindoff, NL
title Sea-ice-driven shallow overturning
title_short Sea-ice-driven shallow overturning
title_full Sea-ice-driven shallow overturning
title_fullStr Sea-ice-driven shallow overturning
title_full_unstemmed Sea-ice-driven shallow overturning
title_sort sea-ice-driven shallow overturning
publisher Nature Publishing Group
publishDate 2016
url https://doi.org/10.1038/ngeo2766
http://ecite.utas.edu.au/109702
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Antarctica
Sea ice
genre_facet Antarc*
Antarctic
Antarctica
Sea ice
op_relation http://ecite.utas.edu.au/109702/1/ngeo2766.pdf
http://dx.doi.org/10.1038/ngeo2766
Bindoff, NL and Hobbs, WR, Sea-ice-driven shallow overturning, Nature Geoscience, 9, (8) pp. 569-570. ISSN 1752-0894 (2016) [Non Refereed Article]
http://ecite.utas.edu.au/109702
op_doi https://doi.org/10.1038/ngeo2766
container_title Nature Geoscience
container_volume 9
container_issue 8
container_start_page 569
op_container_end_page 570
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