Evolution of the snow cover near Zermatt

Zermatt is in the corner of the Sentinel-2 tile 32TLS, which is produced at level 2A by Theia. Hence I could generate the snow maps at 20 m resolution for this area (105 dates from December 2015 to October 2017).

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The glacier outlines are from the Randolph Glacier Inventory 5.0. Snow maps can be useful for glaciologists since the end-of-summer snow line elevation over a glacier is a good proxy of the glacier mass balance [1].



[1] Rabatel, Antoine, Jean-Pierre Dedieu, and Christian Vincent. "Using remote-sensing data to determine equilibrium-line altitude and mass-balance time series: validation on three French glaciers, 1994–2002." Journal of Glaciology 51.175 (2005): 539-546.

[edit Oct. 25, 2017] the animation was updated using the new version of LIS.

Posted under: snow-ice

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