Crevasses detection in Himalayan glaciers using ground-penetrating radar

被引:0
作者
Singh, K. K. [1 ]
Negi, H. S. [1 ]
Ganju, A. [1 ]
Kulkarni, A. V. [2 ]
Kumar, A. [3 ]
Mishra, V. D. [1 ]
Kumar, S. [1 ]
机构
[1] Snow & Avalanche Study Estab, Chandigarh 160036, India
[2] Indian Inst Sci, Divecha Ctr Climate Change, Bangalore 560012, Karnataka, India
[3] Natl Inst Technol, Kurukshetra 136119, Haryana, India
来源
CURRENT SCIENCE | 2013年 / 105卷 / 09期
关键词
Crevasses detection; glaciers; ground-penetrating radar; ICE STREAM-B; EXAMPLES; SHELF;
D O I
暂无
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Identification and mapping of crevasses in glaciated regions is important for safe movement. However, the remote and rugged glacial terrain in the Himalaya poses greater challenges for field data collection. In the present study crevasse signatures were collected from Siachen and Samudra Tapu glaciers in the Indian Himalaya using ground-penetrating radar (GPR). The surveys were conducted using the antennas of 250 MHz frequency in ground mode and 350 MHz in airborne mode. The identified signatures of open and hidden crevasses in GPR profiles collected in ground mode were validated by ground truthing. The crevasse zones and buried boulder areas in a glacier were identified using a combination of airborne GPR profiles and SAR data, and the same have been validated with the high-resolution optical satellite imagery (Cartosat-1) and Survey of India mapsheet. Using multi-sensor data, a crevasse map for Samudra Tapu glacier was prepared. The present methodology can also be used for mapping the crevasse zones in other glaciers in the Himalaya.
引用
收藏
页码:1288 / 1295
页数:8
相关论文
共 20 条
[1]  
[Anonymous], 1980, POLAR REC, DOI [DOI 10.1017/S0032247400002898, 10.1017/S0032247400002898]
[2]   GROUND-PENETRATING RADAR FOR HIGH-RESOLUTION MAPPING OF SOIL AND ROCK STRATIGRAPHY [J].
DAVIS, JL ;
ANNAN, AP .
GEOPHYSICAL PROSPECTING, 1989, 37 (05) :531-551
[3]  
Delaney A J, 2004, 10 INT C GROUND PEN
[4]  
Eder K, 2008, INT ARCH PHOTOGRAMME, V37, P837
[5]  
Gusain H. S., 2009, P INT S SNOW MON AV
[6]  
HAMBREY M., 1978, J GLACIOL, V20, P41, DOI DOI 10.3189/S0022143000021213
[7]   Crevasse patterns and the strain-rate tensor: a high-resolution comparison [J].
Harper, JT ;
Humphrey, NF ;
Pfeffer, WT .
JOURNAL OF GLACIOLOGY, 1998, 44 (146) :68-76
[8]  
Holdsworth G., 1969, Journal of Glaciology, V8, P107, DOI [DOI 10.3189/S0022143000020797, 10.3189/S0022143000020797]
[9]  
JIRACEK G, 1971, ANTARCTIC SNOW ICE S, V16, P199
[10]   Basal crevasses in Larsen C Ice Shelf and implications for their global abundance [J].
Luckman, A. ;
Jansen, D. ;
Kulessa, B. ;
King, E. C. ;
Sammonds, P. ;
Benn, D. I. .
CRYOSPHERE, 2012, 6 (01) :113-123