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DOI10.1126/science.aax2626
How fast will the Antarctic ice sheet retreat?: Feedbacks between glacier retreat and the solid Earth may slow ice loss from Antarctica
Steig E.J.
发表日期2019
ISSN0036-8075
起始页码936
结束页码937
卷号364期号:6444
英文摘要[无可用摘要]
英文关键词sea water; air temperature; feedback mechanism; glacier retreat; global warming; ice retreat; sea ice; solid Earth; acceleration; Antarctica; deglaciation; glacier; ice sheet; ice shelf; priority journal; Review; sea level rise; simulation; topography; water flow; Antarctica; astronomy; feedback system; greenhouse effect; ice cover; Antarctic Ice Sheet; Antarctica; Antarctic Regions; Earth (Planet); Feedback; Global Warming; Ice Cover
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/245594
作者单位Department of Earth and Space Sciences, University of Washington, Seattle, WA 98105, United States
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Steig E.J.. How fast will the Antarctic ice sheet retreat?: Feedbacks between glacier retreat and the solid Earth may slow ice loss from Antarctica[J],2019,364(6444).
APA Steig E.J..(2019).How fast will the Antarctic ice sheet retreat?: Feedbacks between glacier retreat and the solid Earth may slow ice loss from Antarctica.Science,364(6444).
MLA Steig E.J.."How fast will the Antarctic ice sheet retreat?: Feedbacks between glacier retreat and the solid Earth may slow ice loss from Antarctica".Science 364.6444(2019).
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