Fast Recession of a West Antarctic Glacier

Satellite radar interferometry observations of Pine Island Glacier, West Antarctica, reveal that the glacier hinge-line position retreated 1.2 ± 0.3 kilometers per year between 1992 and 1996, which in turn implies that the ice thinned by 3.5 ± 0.9 meters per year. The fast recession of Pine Island G...

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Published in:Science
Main Author: Rignot, E. J.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1998
Subjects:
Online Access:http://dx.doi.org/10.1126/science.281.5376.549
https://www.science.org/doi/pdf/10.1126/science.281.5376.549
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spelling craaas:10.1126/science.281.5376.549 2024-09-15T17:42:47+00:00 Fast Recession of a West Antarctic Glacier Rignot, E. J. 1998 http://dx.doi.org/10.1126/science.281.5376.549 https://www.science.org/doi/pdf/10.1126/science.281.5376.549 en eng American Association for the Advancement of Science (AAAS) Science volume 281, issue 5376, page 549-551 ISSN 0036-8075 1095-9203 journal-article 1998 craaas https://doi.org/10.1126/science.281.5376.549 2024-07-18T04:01:26Z Satellite radar interferometry observations of Pine Island Glacier, West Antarctica, reveal that the glacier hinge-line position retreated 1.2 ± 0.3 kilometers per year between 1992 and 1996, which in turn implies that the ice thinned by 3.5 ± 0.9 meters per year. The fast recession of Pine Island Glacier, predicted to be a possible trigger for the disintegration of the West Antarctic Ice Sheet, is attributed to enhanced basal melting of the glacier floating tongue by warm ocean waters. Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Sheet Pine Island Pine Island Glacier West Antarctica AAAS Resource Center (American Association for the Advancement of Science) Science 281 5376 549 551
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description Satellite radar interferometry observations of Pine Island Glacier, West Antarctica, reveal that the glacier hinge-line position retreated 1.2 ± 0.3 kilometers per year between 1992 and 1996, which in turn implies that the ice thinned by 3.5 ± 0.9 meters per year. The fast recession of Pine Island Glacier, predicted to be a possible trigger for the disintegration of the West Antarctic Ice Sheet, is attributed to enhanced basal melting of the glacier floating tongue by warm ocean waters.
format Article in Journal/Newspaper
author Rignot, E. J.
spellingShingle Rignot, E. J.
Fast Recession of a West Antarctic Glacier
author_facet Rignot, E. J.
author_sort Rignot, E. J.
title Fast Recession of a West Antarctic Glacier
title_short Fast Recession of a West Antarctic Glacier
title_full Fast Recession of a West Antarctic Glacier
title_fullStr Fast Recession of a West Antarctic Glacier
title_full_unstemmed Fast Recession of a West Antarctic Glacier
title_sort fast recession of a west antarctic glacier
publisher American Association for the Advancement of Science (AAAS)
publishDate 1998
url http://dx.doi.org/10.1126/science.281.5376.549
https://www.science.org/doi/pdf/10.1126/science.281.5376.549
genre Antarc*
Antarctic
Antarctica
Ice Sheet
Pine Island
Pine Island Glacier
West Antarctica
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
Pine Island
Pine Island Glacier
West Antarctica
op_source Science
volume 281, issue 5376, page 549-551
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.281.5376.549
container_title Science
container_volume 281
container_issue 5376
container_start_page 549
op_container_end_page 551
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