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- W4313651212 abstract "Himalayan glaciers encompass the highest concentration of ice reserves outside the polar regions. However, the quantitative estimates of ice volume in this vast mountain range are uncertain due to scarcity of field-based thickness measurements. In this chapter, we have compiled and presented up-to-date field-based ice-thickness estimates in the Indian Himalayan Region acquired through multiple geophysical methods, mainly resistivity, seismic, magnetic, and ground penetrating radar (GPR-electromagnetic). It is found that 4 glaciers of the Central and 10 glaciers of the Western Himalaya had direct geophysical measurements, while Zemu Glacier only in the Eastern Himalaya had field-based thickness measurements. After the first ice thickness in 1965, there are 200 records of thickness measurements from Himalayan glaciers that have been recorded to date. Our field-based experience on Satopanth Glacier (Central Himalaya) indicates that serious challenges and difficulties have been faced during GPR data acquisition and processing. In debris-free glaciers, the existing geophysical system (GPR) is well applicable; however, debris-covered glaciers need modified and updated methods because of their uneven surface and englacil debris. Airborne ice sounding radar systems have proved to be one of the best methods to increase thickness measurements in debris-covered rugged Himalayan terrain. The available ice thickness data from different geophysical methods could be combined with the numerical models to update the thickness measurements in the Himalaya." @default.
- W4313651212 created "2023-01-07" @default.
- W4313651212 creator A5051087341 @default.
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- W4313651212 date "2022-12-10" @default.
- W4313651212 modified "2023-10-10" @default.
- W4313651212 title "Glacier Ice Thickness Estimation in Indian Himalaya Using Geophysical Methods" @default.
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- W4313651212 doi "https://doi.org/10.1002/9781119787754.ch20" @default.
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