Not exact matches
So, as the leading
edge melts, this deformation and filling would be first
observed as a thinning of the sheet and, in particular, the trunk or main
ice stream channel, as well as an acceleration of the stream.
This is in fact increasingly
observed around the
edges of Greenland and Antarctica in recent years: outlet glaciers and
ice streams that drain the
ice sheets have greatly accelerated their flow.
Zhang and Lindsay, 4.4 + / -0.5, Modeling The predicted
ice edge in the western Arctic in 2012 is close to that
observed in 2011, while the predicted
ice extent in the eastern Arctic is smaller than in 2011 (Fig. 2).
Bidlot, S. Jacobsen, S. Lehner, P. O. G. Persson and A. L. Pleskachevsky (June 2017): The Potential of TerraSAR - X to
Observe Wind Wave Interaction at the
Ice Edge.
Moulin discharges mapped inside ∼ 52 % of the source
ice watershed for Isortoq, a major proglacial river, totaled ∼ 41 — 98 % of
observed proglacial discharge, highlighting the importance of supraglacial river drainage to true outflow from the
ice edge.
The same changes, increased melting of
ice at the
edges and increased snowfall adding
ice on top, are also
observed in Greenland.