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Variability in ice motion at a land terminating Greenlandic outlet glacier: the role of channelized and distributed drainage systems

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Figure

Fig. 1. (a) Map showing the estimated hydrological catchment of Leverett Glacier (dark grey shading; Bartholomew and others, 2011b; Palmerand others, 2011; Cowton and others, 2012) on the western margin of the Greenland ice sheet (pale grey shading), with
Fig. 3. Schematic depicting the configuration of the hydrological model.
Fig. 4. Melt rate obtained from the UDG at S3 (left axis), scaled to give runoff used as input to the moulin in the hydrological model (right axis).
Table 3. Measurements of supraglacial melt water input at moulin L7
+5

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