A view of Greenland’s ice sheet from the NASA/USGS Landsat 8 satellite, narrated by Dr. Allen Pope. The data enables Dr. Pope to measure the depth of the lakes that form on the surface every summer as the snow and ice melts. The data in this image are from July 12, 2014, and shows the area just south of the Jakobshavn Glacier.
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Aug 17, 2015 • How deep is that icy blue water on Greenland’s ice sheet? Dr. Allen Pope, of the National Snow and Ice Data Center, is using data from the NASA/USGS Landsat 8 satellite to find out. In this video, Dr. Pope shares what he sees when he looks at a Landsat image of the Greenland ice sheet just south of the Jakobshavn Glacier.

Because the lakes are darker than the ice around them, they absorb more energy from the sun. A little bit of melt concentrates in one place, and then melts more, establishing a feedback mechanism accelerating the growth of the lake. When the lakes get big enough they can force open fractures that then drill all the way down to the bed of the glacier, transporting this water to the base where it can temporarily speed up the flow of the ice.

NASA and the U.S. Department of the Interior through the U.S. Geological Survey (USGS) jointly manage the Landsat program, and the USGS preserves a 40-plus-year archive of Landsat images that is freely available over the Internet.
 
 
Reference:

Pope, A., Scambos, T., Moussavi, M., Tedesco, M., Willis, M., Shean, D., Grigsby, S. (2015). "Estimating supraglacial lake depth in western Greenland using Landsat 8 and comparison with other multispectral methods.", The Cryosphere Discuss., pp. 3257-3292 DOI: doi:10.5194/tcd-9-3257-2015

 
 
Further resources:
+ Download the video from the NASA Science Visualization Studio