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DOI10.1126/science.aaz1183
A slip law for glaciers on deformable beds
Zoet L.K.; Iverson N.R.
发表日期2020
ISSN0036-8075
卷号368期号:6486
英文摘要Slip of marine-terminating ice streams over beds of deformable till is responsible for most of the contribution of the West Antarctic Ice Sheet to sea level rise. Flow models of the ice sheet and till-bedded glaciers elsewhere require a law that relates slip resistance, slip velocity, and water pressure at the bed. We present results of experiments in which pressurized ice at its melting temperature is slid over a water-saturated till bed. Steady-state slip resistance increases with slip velocity owing to sliding of ice across the bed, but above a threshold velocity, till shears at its rate-independent Coulomb strength. These results motivate a generalized slip law for glacier-flow models that combines processes of hard-bedded sliding and bed deformation. © 2020 American Association for the Advancement of Science. All rights reserved.
关键词icewaterCoulomb criterionflow modelingglacier flowice sheetsea level changeslidingthresholdArticlecontrolled studyflow rateglacierglacier slipice sheetmelting temperaturepressurepriority journalsteady statestrengthwater flowwater pressureAntarctic Ice SheetAntarcticaWest Antarctic Ice SheetWest Antarctica
语种英语
来源机构Science
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/133588
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Zoet L.K.,Iverson N.R.. A slip law for glaciers on deformable beds[J]. Science,2020,368(6486).
APA Zoet L.K.,&Iverson N.R..(2020).A slip law for glaciers on deformable beds.,368(6486).
MLA Zoet L.K.,et al."A slip law for glaciers on deformable beds".368.6486(2020).
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