of high
resolution airborne lidar imagery as a method to derive glacier velocity for slower moving,
smaller ice masses, using surveys of Midre Lovenbreen, NW Svalbard, from 2003 and 2005.
These data were used by Rees and Arnold (2007) to calculate preliminary estimates of the
glacier velocity. We use three methods; manual
delineation of visible features (e.g. supra-
glacial streams, crevasse
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