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DOI10.1126/science.1072708
Surface melt-induced acceleration of Greenland ice-sheet flow
Zwally H.J.; Abdalati W.; Herring T.; Larson K.; Saba J.; Steffen K.
发表日期2002
ISSN0036-8075
起始页码218
结束页码222
卷号297期号:5579
英文摘要Ice flow at a location in the equilibrium zone of the west-central Greenland Ice Sheet accelerates above the midwinter average rate during periods of summer melting. The near coincidence of the ice acceleration with the duration of surface melting, followed by deceleration after the melting ceases, indicates that glacial sliding is enhanced by rapid migration of surface meltwater to the ice-bedrock interface. Interannual variations in the ice acceleration are correlated with variations in the intensity of the surface melting, with larger increases accompanying higher amounts of summer melting. The indicated coupling between surface melting and ice-sheet flow provides a mechanism for rapid, large-scale, dynamic responses of ice sheets to climate warming.
英文关键词Equilibrium zone; Climate change; Melting; Ice; ice; surface water; global warming; ice flow; ice sheet; melting; meltwater; article; climate change; environmental temperature; Greenland; melting point; priority journal; summer; winter; Greenland
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/246194
作者单位Oceans and Ice Branch, NASA Goddard Space Flight Center, Greenbelt, MD 20771, United States
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Zwally H.J.,Abdalati W.,Herring T.,et al. Surface melt-induced acceleration of Greenland ice-sheet flow[J],2002,297(5579).
APA Zwally H.J.,Abdalati W.,Herring T.,Larson K.,Saba J.,&Steffen K..(2002).Surface melt-induced acceleration of Greenland ice-sheet flow.Science,297(5579).
MLA Zwally H.J.,et al."Surface melt-induced acceleration of Greenland ice-sheet flow".Science 297.5579(2002).
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