ePrints@IIScePrints@IISc Home | About | Browse | Latest Additions | Advanced Search | Contact | Help

Estimation of snow accumulation on Samudra Tapu glacier, Western Himalaya using airborne ground penetrating radar

Singh, K K and Negi, H S and Kumar, A and Kulkarni, A V and Dewali, S K and Datt, P and Ganju, A and Kumar, S (2017) Estimation of snow accumulation on Samudra Tapu glacier, Western Himalaya using airborne ground penetrating radar. In: CURRENT SCIENCE, 112 (6). pp. 1208-1218.

[img] PDF
Cur_Sci_112-6_1208_2017.pdf - Published Version
Restricted to Registered users only

Download (7MB) | Request a copy
Official URL: http://dx.doi.org/10.18520/cs/v112/i06/1208-1218


In this study an airborne ground penetrating radar (GPR) is used to estimate spatial distribution of snow accumulation in the Samudra Tapu glacier (the Great Himalayan Range), Western Himalaya, India. An impulse radar system with 350 MHz antenna was mounted on a helicopter for the estimation of snow depth. The dielectric properties of snow were measured at a representative site (Patseo Observatory) using a snow fork to calibrate GPR data. The snow depths estimated from GPR signal were found to be in good agreement with those measured on ground with an absolute error of 0.04 m. The GPR survey was conducted over Samudra Tapu glacier in March 2009 and 2010. A kriging-based geostatistical interpolation method was used to generate a spatial snow accumulation map of the glacier with the GPR-collected data. The average accumulated snow depth and snow water equivalent (SWE) for a part of the glacier were found to be 2.23 m and 0.624 m for 2009 and 2.06 m and 0.496 m for 2010 respectively. Further, the snow accumulation data were analysed with various topographical parameters such as altitude, aspect and slope. The accumulated snow depth showed good correlation with altitude, having correlation coefficient varying between 0.57 and 0.84 for different parts of the glacier. Higher snow accumulation was observed in the north- and east-facing regions, and decrease in snow accumulation was found with an increase in the slope of the glacier. Thus, in this study we generate snow accumulation/SWE information using airborne GPR in the Himalayan terrain.

Item Type: Journal Article
Additional Information: Copy right for this article belongs to the INDIAN ACAD SCIENCES, C V RAMAN AVENUE, SADASHIVANAGAR, P B #8005, BANGALORE 560 080, INDIA
Department/Centre: Division of Mechanical Sciences > Divecha Centre for Climate Change
Date Deposited: 03 Jun 2017 09:44
Last Modified: 03 Jun 2017 09:44
URI: http://eprints.iisc.ac.in/id/eprint/57123

Actions (login required)

View Item View Item