Abstract
The interaction between large masses of snow and ice with the earth’s climate is of fundamental importance. The strong coupling between the cryosphere, which includes the ice and snow fields, sea ice and permafrost, with the other components of the climatic system cannot be underestimated. Its influence on the global climate acts at long time scales and is a dominant factor in the variation of the planetary albedo (see, for instance, [PO]).
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Rodrigues, J.F., Santos, L. (1997). Some free boundary problems in theorical glaciology. In: Díaz, J.I. (eds) The Mathematics of Models for Climatology and Environment. NATO ASI Series, vol 48. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-60603-8_10
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