Seasonal inflow of warm water onto the southern Weddell Sea continental shelf, Antarctica

To capture the austral summer to winter transition in water mass properties over the southern Weddell Sea continental shelf and slope region Weddell seals were tagged with miniaturized conductivity–temperature–depth sensors in February 2011. During the following 8 months the instruments yielded abou...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Arthun, Marius, Nicholls, Keith, Makinson, Keith, Fedak, Mike, Boehme, Lars
Other Authors: NERC, University of St Andrews. School of Biology, University of St Andrews. Scottish Oceans Institute, University of St Andrews. Marine Alliance for Science & Technology Scotland, University of St Andrews. Sea Mammal Research Unit
Format: Article in Journal/Newspaper
Language:English
Published: 2013
Subjects:
GC
Online Access:http://hdl.handle.net/10023/3370
https://doi.org/10.1029/2012GL052856
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spelling ftstandrewserep:oai:research-repository.st-andrews.ac.uk:10023/3370 2023-07-02T03:30:41+02:00 Seasonal inflow of warm water onto the southern Weddell Sea continental shelf, Antarctica Arthun, Marius Nicholls, Keith Makinson, Keith Fedak, Mike Boehme, Lars NERC University of St Andrews. School of Biology University of St Andrews. Scottish Oceans Institute University of St Andrews. Marine Alliance for Science & Technology Scotland University of St Andrews. Sea Mammal Research Unit 2013-03-01 6 application/pdf http://hdl.handle.net/10023/3370 https://doi.org/10.1029/2012GL052856 eng eng Geophysical Research Letters Arthun , M , Nicholls , K , Makinson , K , Fedak , M & Boehme , L 2012 , ' Seasonal inflow of warm water onto the southern Weddell Sea continental shelf, Antarctica ' , Geophysical Research Letters , vol. 39 , L17601 . https://doi.org/10.1029/2012GL052856 0094-8276 PURE: 21246145 PURE UUID: 9ff465cc-2d58-4b9d-96f8-82d97ef7a624 Scopus: 84865793025 ORCID: /0000-0002-9569-1128/work/47136255 http://hdl.handle.net/10023/3370 https://doi.org/10.1029/2012GL052856 NE/G014833/1 (c) 2012 American Geophysical Union GC Oceanography GC Journal article 2013 ftstandrewserep https://doi.org/10.1029/2012GL052856 2023-06-13T18:31:04Z To capture the austral summer to winter transition in water mass properties over the southern Weddell Sea continental shelf and slope region Weddell seals were tagged with miniaturized conductivity–temperature–depth sensors in February 2011. During the following 8 months the instruments yielded about 9000 temperature–salinity profiles from a previously undersampled area. This allows, for the first time, a description of the seasonality of warm water intrusions onto the shelf. A temperature section across the Filchner Depression and eastern shelf shows a pronounced decrease in warm water inflow from summer to winter, further supported by an almost 3–year long time series from a shelf–break mooring. The seasonal variability is related to the surface wind stress and an associated deepening of the off–shore core of Warm Deep Water. Publisher PDF Peer reviewed Article in Journal/Newspaper Antarc* Antarctica Weddell Sea Weddell Seals University of St Andrews: Digital Research Repository Austral Weddell Weddell Sea Geophysical Research Letters 39 17 n/a n/a
institution Open Polar
collection University of St Andrews: Digital Research Repository
op_collection_id ftstandrewserep
language English
topic GC Oceanography
GC
spellingShingle GC Oceanography
GC
Arthun, Marius
Nicholls, Keith
Makinson, Keith
Fedak, Mike
Boehme, Lars
Seasonal inflow of warm water onto the southern Weddell Sea continental shelf, Antarctica
topic_facet GC Oceanography
GC
description To capture the austral summer to winter transition in water mass properties over the southern Weddell Sea continental shelf and slope region Weddell seals were tagged with miniaturized conductivity–temperature–depth sensors in February 2011. During the following 8 months the instruments yielded about 9000 temperature–salinity profiles from a previously undersampled area. This allows, for the first time, a description of the seasonality of warm water intrusions onto the shelf. A temperature section across the Filchner Depression and eastern shelf shows a pronounced decrease in warm water inflow from summer to winter, further supported by an almost 3–year long time series from a shelf–break mooring. The seasonal variability is related to the surface wind stress and an associated deepening of the off–shore core of Warm Deep Water. Publisher PDF Peer reviewed
author2 NERC
University of St Andrews. School of Biology
University of St Andrews. Scottish Oceans Institute
University of St Andrews. Marine Alliance for Science & Technology Scotland
University of St Andrews. Sea Mammal Research Unit
format Article in Journal/Newspaper
author Arthun, Marius
Nicholls, Keith
Makinson, Keith
Fedak, Mike
Boehme, Lars
author_facet Arthun, Marius
Nicholls, Keith
Makinson, Keith
Fedak, Mike
Boehme, Lars
author_sort Arthun, Marius
title Seasonal inflow of warm water onto the southern Weddell Sea continental shelf, Antarctica
title_short Seasonal inflow of warm water onto the southern Weddell Sea continental shelf, Antarctica
title_full Seasonal inflow of warm water onto the southern Weddell Sea continental shelf, Antarctica
title_fullStr Seasonal inflow of warm water onto the southern Weddell Sea continental shelf, Antarctica
title_full_unstemmed Seasonal inflow of warm water onto the southern Weddell Sea continental shelf, Antarctica
title_sort seasonal inflow of warm water onto the southern weddell sea continental shelf, antarctica
publishDate 2013
url http://hdl.handle.net/10023/3370
https://doi.org/10.1029/2012GL052856
geographic Austral
Weddell
Weddell Sea
geographic_facet Austral
Weddell
Weddell Sea
genre Antarc*
Antarctica
Weddell Sea
Weddell Seals
genre_facet Antarc*
Antarctica
Weddell Sea
Weddell Seals
op_relation Geophysical Research Letters
Arthun , M , Nicholls , K , Makinson , K , Fedak , M & Boehme , L 2012 , ' Seasonal inflow of warm water onto the southern Weddell Sea continental shelf, Antarctica ' , Geophysical Research Letters , vol. 39 , L17601 . https://doi.org/10.1029/2012GL052856
0094-8276
PURE: 21246145
PURE UUID: 9ff465cc-2d58-4b9d-96f8-82d97ef7a624
Scopus: 84865793025
ORCID: /0000-0002-9569-1128/work/47136255
http://hdl.handle.net/10023/3370
https://doi.org/10.1029/2012GL052856
NE/G014833/1
op_rights (c) 2012 American Geophysical Union
op_doi https://doi.org/10.1029/2012GL052856
container_title Geophysical Research Letters
container_volume 39
container_issue 17
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