Sea surface temperature estimation of the South Tasman Rise ...

The Subtropical Front (STF) marking the northern boundary of the Southern Ocean has a steep gradient in sea surface temperature (SST) of approximately 4°C over 0.5° of latitude. Presently, in the region south of Tasmania, the STF lies nominally at 47°S in the summer and 45°S in the winter. We presen...

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Main Authors: Sikes, Elisabeth L, Howard, William R, Samson, Catherine R, Mahan, T S, Robertson, L G, Volkman, John K
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2009
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.831975
https://doi.pangaea.de/10.1594/PANGAEA.831975
id ftdatacite:10.1594/pangaea.831975
record_format openpolar
spelling ftdatacite:10.1594/pangaea.831975 2024-09-15T18:37:03+00:00 Sea surface temperature estimation of the South Tasman Rise ... Sikes, Elisabeth L Howard, William R Samson, Catherine R Mahan, T S Robertson, L G Volkman, John K 2009 application/zip https://dx.doi.org/10.1594/pangaea.831975 https://doi.pangaea.de/10.1594/PANGAEA.831975 en eng PANGAEA https://dx.doi.org/10.1029/2008pa001659 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 article Collection Supplementary Publication Series of Datasets 2009 ftdatacite https://doi.org/10.1594/pangaea.83197510.1029/2008pa001659 2024-08-01T10:57:37Z The Subtropical Front (STF) marking the northern boundary of the Southern Ocean has a steep gradient in sea surface temperature (SST) of approximately 4°C over 0.5° of latitude. Presently, in the region south of Tasmania, the STF lies nominally at 47°S in the summer and 45°S in the winter. We present here SST reconstructions in a latitudinal transect of cores across the South Tasman Rise, southeast of Australia, during the late Quaternary. SST reconstructions are based on two paleotemperature proxies, alkenones and faunal assemblages, which are used to assess past changes in SST in spring and summer. The north-south alignment in core locations allows reconstruction of movement of the STF over the last 100 ka. Surface water temperatures during the last glaciation in this region were ~4°C colder than today. Additional temperature changes greater in magnitude than 4°C seen in individual cores can be attributed to changes in the water mass overlying the core site caused by the movement of the front across that ... : Supplement to: Sikes, Elisabeth L; Howard, William R; Samson, Catherine R; Mahan, T S; Robertson, L G; Volkman, John K (2009): Southern Ocean seasonal temperature and Subtropical Front movement on the South Tasman Rise in the late Quaternary. Paleoceanography, 24(2), PA2201 ... Article in Journal/Newspaper Southern Ocean DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
description The Subtropical Front (STF) marking the northern boundary of the Southern Ocean has a steep gradient in sea surface temperature (SST) of approximately 4°C over 0.5° of latitude. Presently, in the region south of Tasmania, the STF lies nominally at 47°S in the summer and 45°S in the winter. We present here SST reconstructions in a latitudinal transect of cores across the South Tasman Rise, southeast of Australia, during the late Quaternary. SST reconstructions are based on two paleotemperature proxies, alkenones and faunal assemblages, which are used to assess past changes in SST in spring and summer. The north-south alignment in core locations allows reconstruction of movement of the STF over the last 100 ka. Surface water temperatures during the last glaciation in this region were ~4°C colder than today. Additional temperature changes greater in magnitude than 4°C seen in individual cores can be attributed to changes in the water mass overlying the core site caused by the movement of the front across that ... : Supplement to: Sikes, Elisabeth L; Howard, William R; Samson, Catherine R; Mahan, T S; Robertson, L G; Volkman, John K (2009): Southern Ocean seasonal temperature and Subtropical Front movement on the South Tasman Rise in the late Quaternary. Paleoceanography, 24(2), PA2201 ...
format Article in Journal/Newspaper
author Sikes, Elisabeth L
Howard, William R
Samson, Catherine R
Mahan, T S
Robertson, L G
Volkman, John K
spellingShingle Sikes, Elisabeth L
Howard, William R
Samson, Catherine R
Mahan, T S
Robertson, L G
Volkman, John K
Sea surface temperature estimation of the South Tasman Rise ...
author_facet Sikes, Elisabeth L
Howard, William R
Samson, Catherine R
Mahan, T S
Robertson, L G
Volkman, John K
author_sort Sikes, Elisabeth L
title Sea surface temperature estimation of the South Tasman Rise ...
title_short Sea surface temperature estimation of the South Tasman Rise ...
title_full Sea surface temperature estimation of the South Tasman Rise ...
title_fullStr Sea surface temperature estimation of the South Tasman Rise ...
title_full_unstemmed Sea surface temperature estimation of the South Tasman Rise ...
title_sort sea surface temperature estimation of the south tasman rise ...
publisher PANGAEA
publishDate 2009
url https://dx.doi.org/10.1594/pangaea.831975
https://doi.pangaea.de/10.1594/PANGAEA.831975
genre Southern Ocean
genre_facet Southern Ocean
op_relation https://dx.doi.org/10.1029/2008pa001659
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.83197510.1029/2008pa001659
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