Spatial patterns of glacier motion during a high-velocity event: Haut Glacier d'Arolla, Switzerland

被引:73
作者
Mair, D [1 ]
Nienow, P
Willis, I
Sharp, M
机构
[1] Univ Alberta, Dept Earth & Atmospher Sci, Edmonton, AB T6G 2E3, Canada
[2] Univ Cambridge, Dept Geog, Cambridge CB2 3EN, England
[3] Univ Glasgow, Dept Geog & Topog Sci, Glasgow G12 8QQ, Lanark, Scotland
关键词
D O I
10.3189/172756501781832412
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The surface motion of Haut Glacier d'Arolla, Switzerland, was monitored at a high spatial and temporal resolution. Data are analyzed to calculate surface velocities, surface strain rates and the components of the glacier force budget before, during and after an early melt season speed-up or "spring event" We investigate the extent to which variations in glacier motion can be attributed to hydrologically induced local forcing or to non-local forcing transmitted via horizontal stress gradients. Enhanced glacier motion is dependent on a change in the spatial distribution of areas of high drag across the glacier.
引用
收藏
页码:9 / 20
页数:12
相关论文
共 40 条
[1]  
Arnold N, 1998, HYDROL PROCESS, V12, P191, DOI 10.1002/(SICI)1099-1085(199802)12:2<191::AID-HYP571>3.0.CO
[2]  
2-C
[3]   TRANSFER OF BASAL SLIDING VARIATIONS TO THE SURFACE OF A LINEARLY VISCOUS GLACIER [J].
BALISE, MJ ;
RAYMOND, CF .
JOURNAL OF GLACIOLOGY, 1985, 31 (109) :308-318
[5]   Evidence for temporally varying "sticky spots" at the base of Trapridge Glacier, Yukon Territory, Canada [J].
Fischer, UH ;
Clarke, GKC ;
Blatter, H .
JOURNAL OF GLACIOLOGY, 1999, 45 (150) :352-360
[8]   THE CREEP OF POLYCRYSTALLINE ICE [J].
GLEN, JW .
PROCEEDINGS OF THE ROYAL SOCIETY OF LONDON SERIES A-MATHEMATICAL AND PHYSICAL SCIENCES, 1955, 228 (1175) :519-538
[9]  
Gordon S, 1998, HYDROL PROCESS, V12, P105, DOI 10.1002/(SICI)1099-1085(199801)12:1<105::AID-HYP566>3.0.CO
[10]  
2-#