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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American Association for the Advancement of Science (AAAS)
1998
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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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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 |
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Open Polar |
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AAAS Resource Center (American Association for the Advancement of Science) |
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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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1810489535523454976 |