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Supraglacial hydrology of the Greenland Ice Sheet - AntarcticGlaciers.org

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Alexander Island Alexander Island fieldwork Andes antarctica APIS author blogging careers case-study Climate change Conference cosmogenic nuclide dating cryospheric geomorphology dating debris covered glaciers deposition EAIS erosion Fieldwork glacier recession glaciofluvial greenland hydrology ice core ice flow Ice shelves ice stream introductory JRI Juneau lakes landsystem LGM mass balance model moraine patagonia people Pine-Island Post-16 prizes remote sensing resource Rothera science communication sea ice Sea level rise sedimentology storymaps structural glaciology study skills SWW Thwaites Glacier tidewater glacier UK video WAIS water resource wildlife Younger Dryas Antarctic Glaciers 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 supr

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 inland and be active for longer (2-3) . As this meltwater will ultimately end up in the ocean, whether that is by direct evacuation off the ice edge or the eventual channelisation of melt from the en- or sub-glacial systems, it directly

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