The erosive capacity of water is probably more significant.
Here's a couple papers from the Proceedings of the National Academy of Sciences that discuss surface melt, soot and albedo:
Surface Melt-Induced Acceleration of Greenland Ice-Sheet Flow
H. Jay Zwally,1* Waleed Abdalati,2 Tom Herring,3 Kristine Larson,4 Jack Saba,5 Konrad Steffen6
Ice flow at a location in the equilibrium zone of the west-central Greenland Ice Sheet accelerates above the midwinter average rate during periods of summer melting. The near coincidence of the ice acceleration with the duration of surface melting, followed by deceleration after the melting ceases, indicates that glacial sliding is enhanced by rapid migration of surface meltwater to the ice-bedrock interface. Interannual variations in the ice acceleration are correlated with variations in the intensity of the surface melting, with larger increases accompanying higher amounts of summer melting. The indicated coupling between surface melting and ice-sheet flow provides a mechanism for rapid, large-scale, dynamic responses of ice sheets to climate warming.
http://www.sciencemag.org/cgi/content/abstract/297/5579/218Soot climate forcing via snow and ice albedos
James Hansen * , and Larissa Nazarenko *
*National Aeronautics and Space Administration Goddard Institute for Space Studies and Columbia University Earth Institute, 2880 Broadway, New York, NY 10025
Contributed by James Hansen, November 4, 2003
Plausible estimates for the effect of soot on snow and ice albedos (1.5% in the Arctic and 3% in Northern Hemisphere land areas) yield a climate forcing of +0.3 W/m2 in the Northern Hemisphere. The "efficacy" of this forcing is 2, i.e., for a given forcing it is twice as effective as CO2 in altering global surface air temperature. This indirect soot forcing may have contributed to global warming of the past century, including the trend toward early springs in the Northern Hemisphere, thinning Arctic sea ice, and melting land ice and permafrost. If, as we suggest, melting ice and sea level rise define the level of dangerous anthropogenic interference with the climate system, then reducing soot emissions, thus restoring snow albedos to pristine high values, would have the double benefit of reducing global warming and raising the global temperature level at which dangerous anthropogenic interference occurs. However, soot contributions to climate change do not alter the conclusion that anthropogenic greenhouse gases have been the main cause of recent global warming and will be the predominant climate forcing in the future.
http://www.pnas.org/cgi/content/abstract/101/2/423