Glacier surge and lake outburst observed by TanDEM-X, Sentinel 1A and LandSat 8.

An entire cycle of the periodic instability forming a surging glacier could be observed by TanDEM-X, Sentinel-1A and LandSat 8 satellite data in an excellent interdisciplinary work of Vanessa Round.

by Muhammad Adnan Siddique

Kyagar Glacier blocks the riverbed of the Upper Shaksgam Valley, Karakorum, and occasionally triggers the formation of an ice-dammed lake, causing destructive floods. A sudden increase of the glacier velocity (glacier surge) caused dramatic ice thickening which was measured by TanDEM-X to exceed 100 meters at the terminus. The glacier thickening initiated the formation of a lake, which exceeded 45 million m3 before draining in less than one day at the end of July 2015. Precursors of the lake-drainage could be identified in Sentinel 1A data and local population could successfully be warned.

The excellent Master Thesis of Vanessa Round formed an integrative picture of the ice-dynamics which drive the periodic instability of the glacier and allows forecasting future flood events.

Enlarged view: Ice dynamics of Kyagar glacier
TanDEM-X data reveal the ice dynamics during the surge: (a): The excess mass in the accumulation area (blue) got unstable and was moved within 2 years into the retreated tongue (red) of the glacier. (b): after the surge, the glacier was close to its initial state in 2000.
Enlarged view: Velocity fields of the ice at the glacier terminus
Three velocity fields of the ice at the glacier terminus calculated from pairs of optical images from the Kyagar station.
Enlarged view: Outburst of the glacier
TerraSAR-X images show the outburst of the glacier lake on 27.07.2015.
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