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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Bibliographic Details
Main Author: Rignot, EJ
Format: Article in Journal/Newspaper
Language:unknown
Published: eScholarship, University of California 1998
Subjects:
Online Access:https://escholarship.org/uc/item/2kp8m2q6
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spelling 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
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