DOI: 10.5194/tc-10-1915-2016
Scopus记录号: 2-s2.0-84986292175
论文题名: Sliding of temperate basal ice on a rough, hard bed: Creep mechanisms, pressure melting, and implications for ice streaming
作者: Krabbendam M
刊名: Cryosphere
ISSN: 19940416
出版年: 2016
卷: 10, 期: 5 起始页码: 1915
结束页码: 1932
语种: 英语
英文关键词: advection
; basal ice
; basal melting
; bedrock
; creep
; grain boundary
; heat flow
; ice stream
; meltwater
; sliding
; Arctic
; Greenland
; Calluna vulgaris
英文摘要: Basal ice motion is crucial to ice dynamics of ice sheets. The classic Weertman model for basal sliding over bedrock obstacles proposes that sliding velocity is controlled by pressure melting and/or ductile flow, whichever is the fastest; it further assumes that pressure melting is limited by heat flow through the obstacle and ductile flow is controlled by standard power-law creep. These last two assumptions, however, are not applicable if a substantial basal layer of temperate (T ~ Tmelt) ice is present. In that case, frictional melting can produce excess basal meltwater and efficient water flow, leading to near-thermal equilibrium. Higherature ice creep experiments have shown a sharp weakening of a factor 5-10 close to Tmelt, suggesting standard power-law creep does not operate due to a switch to melt-assisted creep with a possible component of grain boundary melting. Pressure melting is controlled by meltwater production, heat advection by flowing meltwater to the next obstacle and heat conduction through ice/rock over half the obstacle height. No heat flow through the obstacle is required. Ice streaming over a rough, hard bed, as possibly in the Northeast Greenland Ice Stream, may be explained by enhanced basal motion in a thick temperate ice layer. © Author(s) 2016. CC Attribution 3.0 License. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/75090
Appears in Collections: 影响、适应和脆弱性 气候变化与战略
There are no files associated with this item.
作者单位: British Geological Survey, Lyell Centre, Research Avenue South, Edinburgh, United Kingdom
Recommended Citation:
Krabbendam M. Sliding of temperate basal ice on a rough, hard bed: Creep mechanisms, pressure melting, and implications for ice streaming[J]. Cryosphere,2016-01-01,10(5)