DOI: | 10.1002/2015GL064195
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论文题名: | Antarctic ice rise formation, evolution, and stability |
作者: | Favier L.; Pattyn F.
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刊名: | Geophysical Research Letters
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ISSN: | 0094-9096
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EISSN: | 1944-8827
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出版年: | 2015
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卷: | 42, 期:11 | 起始页码: | 4456
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结束页码: | 4463
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语种: | 英语
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英文关键词: | deglaciation
; ice rise
; modeling
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Scopus关键词: | Earth sciences
; Geophysics
; Models
; Continental shelves
; Deglaciations
; Grounding line
; Ice flow
; Ice sheet
; Ice shelves
; Numerical results
; Steady state
; Ice
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英文摘要: | Antarctic ice rises originate from the contact between ice shelves and one of the numerous topographic highs emerging from the edge of the continental shelf. While investigations of the Raymond effect indicate their millennial-scale stability, little is known about their formation and their role in ice shelf stability. Here we present for the first time the simulation of an ice rise using the BISICLES model. The numerical results successfully reproduce several field-observable features, such as the substantial thinning downstream of the ice rise and the successive formation of a promontory and ice rise with stable radial ice flow center, showing that ice rises are formed during the ice sheet deglaciation. We quantify the ice rise buttressing effect, found to be mostly transient, delaying grounding line retreat significantly but resulting in comparable steady state positions. We demonstrate that ice rises are key in controlling simulations of Antarctic deglaciation. ©2015. American Geophysical Union. All Rights Reserved. |
URL: | https://www.scopus.com/inward/record.uri?eid=2-s2.0-84934444048&doi=10.1002%2f2015GL064195&partnerID=40&md5=c2a5b0b22ea466264df5a4e710a887b8
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Citation statistics: |
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资源类型: | 期刊论文
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标识符: | http://119.78.100.158/handle/2HF3EXSE/8712
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Appears in Collections: | 科学计划与规划 气候变化与战略
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作者单位: | Laboratoire de Glaciologie, Université Libre de Bruxelles, Brussels, Belgium
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Recommended Citation: |
Favier L.,Pattyn F.. Antarctic ice rise formation, evolution, and stability[J]. Geophysical Research Letters,2015-01-01,42(11).
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