Supraglacial hydrology of the Greenland Ice Sheet
By Lauren Rawlins, University of York Since the early 1990’s, the amount of meltwater on the Greenland Ice Sheet has dramatically increased due to rising air temperatures from climatic warming and darkening of the ice surface (1). Observations from satellite imagery over this time have seen the supraglacial hydrology system become more extensive, form further …
Supraglacial hydrology of the Greenland Ice Sheet Read More »