Key points are not available for this paper at this time.
The formation of an ice layer at the base of to dissipate the latent heat released by the reHigh Arctic snowpacks is due to a refreezing freezing process, but through such latent heat of the meltwater percolating to the snow- transfer the warming of the active layer is acground interface. A cold substrate is required celerated.
Woo et al. (Fri,) studied this question.