Inland Thinning of Pine Island Glacier, West Antarctica

The Pine Island Glacier (PIG) transports 69 cubic kilometers of ice each year from ∼10% of the West Antarctic Ice Sheet (WAIS). It is possible that a retreat of the PIG may accelerate ice discharge from the WAIS interior. Satellite altimetry and interferometry show that the grounded PIG thinned by u...

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Published in:Science
Main Authors: Shepherd, Andrew, Wingham, Duncan J., Mansley, Justin A. D., Corr, Hugh F. J.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 2001
Subjects:
Online Access:http://dx.doi.org/10.1126/science.291.5505.862
https://www.science.org/doi/pdf/10.1126/science.291.5505.862
id craaas:10.1126/science.291.5505.862
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spelling craaas:10.1126/science.291.5505.862 2024-09-15T17:41:13+00:00 Inland Thinning of Pine Island Glacier, West Antarctica Shepherd, Andrew Wingham, Duncan J. Mansley, Justin A. D. Corr, Hugh F. J. 2001 http://dx.doi.org/10.1126/science.291.5505.862 https://www.science.org/doi/pdf/10.1126/science.291.5505.862 en eng American Association for the Advancement of Science (AAAS) Science volume 291, issue 5505, page 862-864 ISSN 0036-8075 1095-9203 journal-article 2001 craaas https://doi.org/10.1126/science.291.5505.862 2024-08-01T04:01:11Z The Pine Island Glacier (PIG) transports 69 cubic kilometers of ice each year from ∼10% of the West Antarctic Ice Sheet (WAIS). It is possible that a retreat of the PIG may accelerate ice discharge from the WAIS interior. Satellite altimetry and interferometry show that the grounded PIG thinned by up to 1.6 meters per year between 1992 and 1999, affecting 150 kilometers of the inland glacier. The thinning cannot be explained by short-term variability in accumulation and must result from glacier dynamics. 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 291 5505 862 864
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description The Pine Island Glacier (PIG) transports 69 cubic kilometers of ice each year from ∼10% of the West Antarctic Ice Sheet (WAIS). It is possible that a retreat of the PIG may accelerate ice discharge from the WAIS interior. Satellite altimetry and interferometry show that the grounded PIG thinned by up to 1.6 meters per year between 1992 and 1999, affecting 150 kilometers of the inland glacier. The thinning cannot be explained by short-term variability in accumulation and must result from glacier dynamics.
format Article in Journal/Newspaper
author Shepherd, Andrew
Wingham, Duncan J.
Mansley, Justin A. D.
Corr, Hugh F. J.
spellingShingle Shepherd, Andrew
Wingham, Duncan J.
Mansley, Justin A. D.
Corr, Hugh F. J.
Inland Thinning of Pine Island Glacier, West Antarctica
author_facet Shepherd, Andrew
Wingham, Duncan J.
Mansley, Justin A. D.
Corr, Hugh F. J.
author_sort Shepherd, Andrew
title Inland Thinning of Pine Island Glacier, West Antarctica
title_short Inland Thinning of Pine Island Glacier, West Antarctica
title_full Inland Thinning of Pine Island Glacier, West Antarctica
title_fullStr Inland Thinning of Pine Island Glacier, West Antarctica
title_full_unstemmed Inland Thinning of Pine Island Glacier, West Antarctica
title_sort inland thinning of pine island glacier, west antarctica
publisher American Association for the Advancement of Science (AAAS)
publishDate 2001
url http://dx.doi.org/10.1126/science.291.5505.862
https://www.science.org/doi/pdf/10.1126/science.291.5505.862
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 291, issue 5505, page 862-864
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.291.5505.862
container_title Science
container_volume 291
container_issue 5505
container_start_page 862
op_container_end_page 864
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