Regional representation of glaciers in Chandra Basin region, western Himalaya, India
Author(s) -
Pratima Pandey,
Sajid Ali,
AL. Ramanathan,
P. K. Champati Ray,
G. Venkataraman
Publication year - 2016
Publication title -
geoscience frontiers
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.842
H-Index - 57
eISSN - 2588-9192
pISSN - 1674-9871
DOI - 10.1016/j.gsf.2016.06.006
Subject(s) - glacier , geology , structural basin , precipitation , glacier mass balance , accumulation zone , glacier morphology , physical geography , climatology , geomorphology , geography , meteorology , cryosphere , ice stream , sea ice
Hamtah and Chhota Shigri are two nearby, well monitored glaciers of western Himalaya, lying in the same climatic zone and driven by the same climatic conditions. In this study, topographical characteristics of both the glacier have been explored to understand the role of topography in controlling the glacier response. Further, their topographical characteristics and possible response towards climatic variations have been compared with each other and also with that of the other glaciers in the basin to find out the suitability of these two glaciers to be considered as representative of the region. Multi sensor and multi temporal remote sensing data have been used to carry out to fulfill the objectives. It is found that being in the same climatic zone, the mean accumulation area ratio of Chhota Shigri is 54% and Hamtah is 11% between 1980 and 2014. In comparison to Hamtah, Chhota Shigri glacier has a small upslope area, low compactness ratio indicating the ability of the glacier to receive direct precipitation and solar radiation. The analysis revealed that the Chhota Shigri glacier has a closer resemblance with the other glaciers in the region than Hamtah glacier. Also, the topographical settings of Chhota Shigri glacier are suitable for recording and reflecting year-to-year climatic variations
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