The Effect of Firn-Aquifer Drainage on the Greenland Subglacial System or Subglacial Efficiency and Storage Modified by the Temporal Pattern of High-Elevation Meltwater Input

Ice flow in marginal region of the Greenland Ice Sheet dynamically responds to summer melting as surface meltwater is routed through the supraglacial hydrologic system to the bed of the ice sheet via crevasses and moulins. Given the expected increases in surface melt production and extent, and the p...

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Bibliographic Details
Main Authors: Poinar, Kristin, Dow, Christine F., Andrews, Lauren C., Nowicki, Sophie M.
Format: Other/Unknown Material
Language:unknown
Published: 2017
Subjects:
Online Access:http://hdl.handle.net/2060/20180000626