中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
The bedrock topography of Starbuck Glacier, Antarctic Peninsula, as determined by radio-echo soundings and flow modeling (SCI)

文献类型:期刊论文

作者Farinotti D. ; King E. C. ; Albrecht A. ; Huss M. ; Gudmundsson G. H.
刊名Annals of Glaciology
出版日期2014
卷号55期号:67页码:22-28
英文摘要A glacier-wide ice-thickness distribution and bedrock topography is presented for Starbuck Glacier, Antarctic Peninsula. The results are based on 90 km of ground-based radio-echo sounding lines collected during the 2012/13 field season. Cross-validation with ice-thickness measurements provided by NASA's IceBridge project reveals excellent agreement. Glacier-wide estimates are derived using a model that calculates distributed ice thickness, calibrated with the radio-echo soundings. Additional constraints are obtained from in situ ice flow-speed measurements and the surface topography. The results indicate a reverse-sloped bed extending from a riegel occurring similar to 5 km upstream of the current grounding line. The deepest parts of the glacier are as much as 500 m below sea level. The calculated total volume of 80.7 +/- 7.2 km(3) corresponds to an average ice thickness of 312 +/- 30 m.
收录类别SCI
公开日期2015-12-24
源URL[http://ir.casnw.net/handle/362004/25112]  
专题寒区旱区环境与工程研究所_中科院寒区旱区环境与工程研究所(未分类)_期刊论文
推荐引用方式
GB/T 7714
Farinotti D.,King E. C.,Albrecht A.,et al. The bedrock topography of Starbuck Glacier, Antarctic Peninsula, as determined by radio-echo soundings and flow modeling (SCI)[J]. Annals of Glaciology,2014,55(67):22-28.
APA Farinotti D.,King E. C.,Albrecht A.,Huss M.,&Gudmundsson G. H..(2014).The bedrock topography of Starbuck Glacier, Antarctic Peninsula, as determined by radio-echo soundings and flow modeling (SCI).Annals of Glaciology,55(67),22-28.
MLA Farinotti D.,et al."The bedrock topography of Starbuck Glacier, Antarctic Peninsula, as determined by radio-echo soundings and flow modeling (SCI)".Annals of Glaciology 55.67(2014):22-28.

入库方式: OAI收割

来源:寒区旱区环境与工程研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。