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DOI10.1126/science.291.5505.862
Inland thinning of Pine Island Glacier, West Antarctica
Shepherd A.; Wingham D.J.; Mansley J.A.D.; Corr H.F.J.
发表日期2001
ISSN0036-8075
起始页码862
结束页码864
卷号291期号:5505
英文摘要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.
英文关键词ice; glacier dynamics; ice thickness; interferometry; satellite altimetry; Antarctica; article; dynamics; geography; interferometry; priority journal
语种英语
来源期刊Science
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/245455
作者单位Ctr. for Polar Observ. and Modelling, Dept. of Space and Climate Physics, University College London, 17 Gordon Street, London, WC1H 0AH, United Kingdom
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Shepherd A.,Wingham D.J.,Mansley J.A.D.,et al. Inland thinning of Pine Island Glacier, West Antarctica[J],2001,291(5505).
APA Shepherd A.,Wingham D.J.,Mansley J.A.D.,&Corr H.F.J..(2001).Inland thinning of Pine Island Glacier, West Antarctica.Science,291(5505).
MLA Shepherd A.,et al."Inland thinning of Pine Island Glacier, West Antarctica".Science 291.5505(2001).
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