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 Isla...
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1998
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ftcdlib:oai:escholarship.org/ark:/13030/qt2kp8m2q6 2023-05-15T14:02:50+02:00 Fast recession of a west antarctic glacier Rignot, EJ 549 - 551 1998-07-01 application/pdf https://escholarship.org/uc/item/2kp8m2q6 unknown eScholarship, University of California qt2kp8m2q6 https://escholarship.org/uc/item/2kp8m2q6 CC-BY CC-BY Science (New York, N.Y.), vol 281, iss 5376 General Science & Technology article 1998 ftcdlib 2020-02-07T23:53:28Z 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 University of California: eScholarship Antarctic Pine Island Glacier ENVELOPE(-101.000,-101.000,-75.000,-75.000) West Antarctic Ice Sheet West Antarctica |
institution |
Open Polar |
collection |
University of California: eScholarship |
op_collection_id |
ftcdlib |
language |
unknown |
topic |
General Science & Technology |
spellingShingle |
General Science & Technology Rignot, EJ Fast recession of a west antarctic glacier |
topic_facet |
General Science & Technology |
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, EJ |
author_facet |
Rignot, EJ |
author_sort |
Rignot, EJ |
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 |
eScholarship, University of California |
publishDate |
1998 |
url |
https://escholarship.org/uc/item/2kp8m2q6 |
op_coverage |
549 - 551 |
long_lat |
ENVELOPE(-101.000,-101.000,-75.000,-75.000) |
geographic |
Antarctic Pine Island Glacier West Antarctic Ice Sheet West Antarctica |
geographic_facet |
Antarctic Pine Island Glacier West Antarctic Ice Sheet West Antarctica |
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 (New York, N.Y.), vol 281, iss 5376 |
op_relation |
qt2kp8m2q6 https://escholarship.org/uc/item/2kp8m2q6 |
op_rights |
CC-BY |
op_rightsnorm |
CC-BY |
_version_ |
1766273246327472128 |