Indian researchers have found a seasonal advancement in 220 surge-type glaciers in the Karakoram Range of Ladakh.
About Surge Type Glaciers:
Glacial surges are short-lived events where a glacier can advance substantially, moving at velocities up to 100 times faster than normal.
Until recently, most glaciologists believed that a glacier’s physical characteristics, such as its thickness and shape, and the properties of the terrain it sits on determining whether it can surge.
Now, it is proved to believe an external factor also plays a major role: water from precipitation and melting.
Pooling on the surface, it can infiltrate the glacier through crevasses and reach its base, warming, lubricating, and, ultimately, releasing the ice.
Why there is a concern?
The behaviour of these glaciers, which represent 40% of the total glaciated area of the Karakoram, goes against the normal trend.
Surging of glaciers is potentially catastrophic as it can lead to the destruction of villages, roads and bridges.
It can also advance across a river valley and form the ice-dammed lake.
These lakes can form catastrophic outburst floods.
Therefore, monitoring of glacier surges, ice-dammed lake formation, and drainage is of paramount importance.