Glacier Surface Velocities in the Chandrabhaga Massif, Western Himalaya (India) Derived Using COSI-Corr From Landsat Images
Abstract Himalayan glaciers act as a storehouse of freshwater outside the polar region and sustain the flow of several Asia’s major river systems, such as the Ganges, Indus, and Brahmaputra. Glaciers in High Mountain Asia are likely to be affected by climate change, posing a threat to the future water supply. Frequent mapping and monitoring of these glaciers are in urgent need to assess the future water storage and glacier-climate interaction. In this context, mapping and monitoring of surface velocity can help to infer the health of a glacier. However, systematic assessment of glacier surface velocity is limited to fewer basins or individual glaciers in the Himalaya. Here, I have characterized the spatial and temporal velocity variations of glaciers in the Chandrabhaga massif (CBM) using Landsat time-series data spanning nearly the last three decades (1992-2019). Rigorous post-processing was performed to improve the accuracy of remote sensing derived velocity products. Glaciers showed heterogeneous spatial and temporal velocity patterns based on morphological characteristics and topographical settings. Heavily debris-covered tongues showed nearly stagnant flow (<10 m/yr) while maximum velocity (>60 m/yr) was observed for clean glaciers with steep gradients and crevasses. Surface velocity near the terminus of the lake terminating glaciers was almost double than land terminating debris-covered tongues (32.5 m/yr vs. 12.6 m/yr). An increasing trend in surface velocity is attributed to the rising trend in air temperature in western Himalaya.