Calibrated Seismic Imaging of Eddy-Dominated Warm-Water Transport Across the Bellingshausen Sea, Southern Ocean ...

AbstractSeismic reflection images of thermohaline circulation from the Bellingshausen Sea, adjacent to the West Antarctica Peninsula, were acquired during February 2015. This survey shows that bright reflectivity occurs throughout the upper 300 m. By calibrating these seismic images with coeval hydr...

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Bibliographic Details
Main Authors: Gunn, KL, White, NJ, Larter, RD, Caulfield, CP
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union (AGU) 2018
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.24608
https://www.repository.cam.ac.uk/handle/1810/277319
id ftdatacite:10.17863/cam.24608
record_format openpolar
spelling ftdatacite:10.17863/cam.24608 2024-02-04T09:52:33+01:00 Calibrated Seismic Imaging of Eddy-Dominated Warm-Water Transport Across the Bellingshausen Sea, Southern Ocean ... Gunn, KL White, NJ Larter, RD Caulfield, CP 2018 https://dx.doi.org/10.17863/cam.24608 https://www.repository.cam.ac.uk/handle/1810/277319 en eng American Geophysical Union (AGU) seismic oceanography Bellingshausen Sea warm-core eddies ice-shelf basal melt Antarctic Slope Front Article ScholarlyArticle JournalArticle article-journal 2018 ftdatacite https://doi.org/10.17863/cam.24608 2024-01-05T16:32:48Z AbstractSeismic reflection images of thermohaline circulation from the Bellingshausen Sea, adjacent to the West Antarctica Peninsula, were acquired during February 2015. This survey shows that bright reflectivity occurs throughout the upper 300 m. By calibrating these seismic images with coeval hydrographic measurements, intrusion of warm water features onto the continental shelf at Marguerite and Belgica Troughs is identified and characterized. These features have distinctive lens‐shaped patterns of reflectivity with lengths of 0.75–11.00 km and thicknesses of 100–150 m, suggesting that they are small mesoscale to submesoscale eddies. Abundant eddies are observed along a transect that crosses Belgica Trough. Near Alexander Island Drift, a large, of order km 3 , bowl‐like feature, that may represent an anticyclonic Taylor column, is imaged on a pair of orthogonal images. A modified iterative procedure is used to convert seismic imagery into maps of temperature that enable the number and size of eddies being ... Article in Journal/Newspaper Alexander Island Antarc* Antarctic Antarctica Bellingshausen Sea Ice Shelf Southern Ocean West Antarctica DataCite Metadata Store (German National Library of Science and Technology) Antarctic Southern Ocean West Antarctica Bellingshausen Sea Marguerite ENVELOPE(141.378,141.378,-66.787,-66.787) Alexander Island ENVELOPE(-69.895,-69.895,-71.287,-71.287)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic seismic oceanography
Bellingshausen Sea
warm-core eddies
ice-shelf basal melt
Antarctic Slope Front
spellingShingle seismic oceanography
Bellingshausen Sea
warm-core eddies
ice-shelf basal melt
Antarctic Slope Front
Gunn, KL
White, NJ
Larter, RD
Caulfield, CP
Calibrated Seismic Imaging of Eddy-Dominated Warm-Water Transport Across the Bellingshausen Sea, Southern Ocean ...
topic_facet seismic oceanography
Bellingshausen Sea
warm-core eddies
ice-shelf basal melt
Antarctic Slope Front
description AbstractSeismic reflection images of thermohaline circulation from the Bellingshausen Sea, adjacent to the West Antarctica Peninsula, were acquired during February 2015. This survey shows that bright reflectivity occurs throughout the upper 300 m. By calibrating these seismic images with coeval hydrographic measurements, intrusion of warm water features onto the continental shelf at Marguerite and Belgica Troughs is identified and characterized. These features have distinctive lens‐shaped patterns of reflectivity with lengths of 0.75–11.00 km and thicknesses of 100–150 m, suggesting that they are small mesoscale to submesoscale eddies. Abundant eddies are observed along a transect that crosses Belgica Trough. Near Alexander Island Drift, a large, of order km 3 , bowl‐like feature, that may represent an anticyclonic Taylor column, is imaged on a pair of orthogonal images. A modified iterative procedure is used to convert seismic imagery into maps of temperature that enable the number and size of eddies being ...
format Article in Journal/Newspaper
author Gunn, KL
White, NJ
Larter, RD
Caulfield, CP
author_facet Gunn, KL
White, NJ
Larter, RD
Caulfield, CP
author_sort Gunn, KL
title Calibrated Seismic Imaging of Eddy-Dominated Warm-Water Transport Across the Bellingshausen Sea, Southern Ocean ...
title_short Calibrated Seismic Imaging of Eddy-Dominated Warm-Water Transport Across the Bellingshausen Sea, Southern Ocean ...
title_full Calibrated Seismic Imaging of Eddy-Dominated Warm-Water Transport Across the Bellingshausen Sea, Southern Ocean ...
title_fullStr Calibrated Seismic Imaging of Eddy-Dominated Warm-Water Transport Across the Bellingshausen Sea, Southern Ocean ...
title_full_unstemmed Calibrated Seismic Imaging of Eddy-Dominated Warm-Water Transport Across the Bellingshausen Sea, Southern Ocean ...
title_sort calibrated seismic imaging of eddy-dominated warm-water transport across the bellingshausen sea, southern ocean ...
publisher American Geophysical Union (AGU)
publishDate 2018
url https://dx.doi.org/10.17863/cam.24608
https://www.repository.cam.ac.uk/handle/1810/277319
long_lat ENVELOPE(141.378,141.378,-66.787,-66.787)
ENVELOPE(-69.895,-69.895,-71.287,-71.287)
geographic Antarctic
Southern Ocean
West Antarctica
Bellingshausen Sea
Marguerite
Alexander Island
geographic_facet Antarctic
Southern Ocean
West Antarctica
Bellingshausen Sea
Marguerite
Alexander Island
genre Alexander Island
Antarc*
Antarctic
Antarctica
Bellingshausen Sea
Ice Shelf
Southern Ocean
West Antarctica
genre_facet Alexander Island
Antarc*
Antarctic
Antarctica
Bellingshausen Sea
Ice Shelf
Southern Ocean
West Antarctica
op_doi https://doi.org/10.17863/cam.24608
_version_ 1789959757462765568