6. One paragraph description of your model (e.g. abstract from report or paper); CROCUS is a one-dimensional model. The snow cover is represented as a pile of layers parallel to the ground. Energy exchanges are projected orthogonally to the slope. The model describes the evolution of the internal state of the snow cover as a function of meteorological conditions. The variables describing the snow cover are temperature, density, liquid water content, snow type of each layer. The thickness and number of layers are adjusted by the model in order that the numerical layers match the natural layers. The model simulate the heat conduction, melting/refreezing of snow layers, settlement, metamorphism, percolation. The originality of the model is that it simulates the snow metamorphism with experimental laws from cold laboratory. The snow grains are characterized by their sizes and types. This allows to calculate an accurate albedo of the snow cover. 50. Please provide references relevant to the model description and use. Brun E., Martin E., Simon V., Gendre C., Coleou C. (1989): "An energy and mass model of snow cover suitable for operational avalanche forecasting", J. of Glaciol., Vol 35, N°121, p333-342. Durand Y., Brun E., Merindol L., Guyomarc'h G., Lesaffre B., Martin E. (1993): "A meteorological estimation of relevant parameters for snow models", Annals of Glaciol., Vol 18, p 65-71. Braun L., Brun E., Durand Y., Martin E. Tourasse P (1994) : "Simulation of discharge using different method of meteorological data distribution, basin discretization and snow modelling", Nordic Hydrology, Vol 25, NO 1/2, p 129-144. Martin E., Brun E., Durand Y. (1994) : "Sensitivity of the French Alps snow cover to the variation of climatic variables", Annales Geophysicae, 12, p 469-477. Brun E., Durand Y., Martin E., Braun L. (1994) : "Snow modelling as an efficient tool to simulate snow cover evolution at different spatial scales", IAHS publication n° 223, p 163-176. Martin E., Timbal B., Brun E. (1997) : "Downscaling of general circulation models outputs : simulation of the snow climatology of the French Alps. Sensitivity to climate changes", Climate Dynamics, 13, 45-56.