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Satellitter skaffer vished om Himalayas gletsjere
 
4 Februar 2010

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This animation, comprised of two images acquired by Landsat’s Thematic Mapper on 15 November 1990 and Enhanced Thematic Mapper plus 1 August 2001 (colourful), illustrates 11 years of glacier change in the Garwhal Himalaya to the northeast of Gangotri Glacier (the area covered is 33 km x 22 km). While most of the smaller and debris-free glaciers show considerable retreat in this period, the larger glaciers with completely debris-covered glacier tongues have not changed much. At several locations pro-glacial lakes have increased in size. Several glaciers at lower elevations are nearly free of snow in the August image, indicating a negative mass balance in that year.

Credits: Landsat scenes provided by U.S. Geological Survey and processed in the framework of the ESA GlobGlacier project by Frank Paul (Dept. of Geography, University of Zurich).
 
 
Surface velocity field for the Baltoro Glacier
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Surface velocity field for the Baltoro Glacier in Pakistan based on six Envisat Advanced Synthetic Aperture Radar images taken from 2003 to 2008. The analysis of mutli-temporal data such as these allows changes in the glacier velocity pattern to be detected accurately and quickly. Inset: Centreline velocity profile; location as depicted by dashed yellow line in main image. Note the gradual increase in flow with distance from the terminus, as is common on debris-covered glaciers, and the velocity maximum at Concordia, which is associated with the confluence of the two major tributary glaciers, the Godwin Austen Glacier and the Baltoro South Glacier.

Credits: Dr Duncan Quincey, Institute of Geography and Earth Science, Aberystwyth University (UK)
 
 
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