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DOI10.1126/science.1070942
Rapid bottom melting widespread near antarctic ice sheet grounding lines
Rignot E.; Jacobs S.S.
发表日期2002
ISSN0036-8075
起始页码2020
结束页码2023
卷号296期号:5575
英文摘要As continental ice from Antarctica reaches the grounding line and begins to float, its underside melts into the ocean. Results obtained with satellite radar interferometry reveal that bottom melt rates experienced by large outlet glaciers near their grounding lines are far higher than generally assumed. The melting rate is positively correlated with thermal forcing, increasing by 1 meter per year for each 0.1°C rise in ocean temperature. Where deep water has direct access to grounding lines, glaciers and ice shelves are vulnerable to ongoing increases in ocean temperature.
英文关键词Atmospheric temperature; Glaciers; Interferometry; Radar; Sea ice; Melting rates; Thermal forcing; Glacial geology; sea water; grounding line; ice sheet; ice-ocean interaction; melting; satellite data; Antarctica; article; correlation analysis; glacier; interferometry; melting point; priority journal; sea; sea ice; water temperature; Antarctica
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/245225
作者单位Jet Propulsion Laboratory, California Institute of Technology, Mail Stop 300-235, Pasadena, CA 91109-8099, United States
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Rignot E.,Jacobs S.S.. Rapid bottom melting widespread near antarctic ice sheet grounding lines[J],2002,296(5575).
APA Rignot E.,&Jacobs S.S..(2002).Rapid bottom melting widespread near antarctic ice sheet grounding lines.Science,296(5575).
MLA Rignot E.,et al."Rapid bottom melting widespread near antarctic ice sheet grounding lines".Science 296.5575(2002).
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