Verhalten abseits der Piste Avalanche accidents Wissenswertes über Lawinen Literatur Kernteam Lawinenausbildung Exceptional avalanche situations
At the core of the Alpine3D-model, is the SNOWPACK model, a physically based, energy balance model for a 1D soil/snow/canopy column. This provides a very detailed description of the snow stratigraphy and a very good evaluation of the mass and energy balance. In Alpine3D this 1D energy balance is performed for each pixel of the domain (therefore it is a distributed SNOWPACK simulation) and for one time step (usually one hour). Any quantity that the user would like to get out of the simulation can be written out from this module.
In order to perform a SNOWPACK simulation at every pixel of the domain, it is necessary to get the meteorological forcing for each pixel. But the measured meteorological parameters are usually measured by a set of stations, which means that the data is available at a set of points. Interpolating these points measurements to every pixels of the domain is performed by the means of statistical interpolations with MeteoIO. If the forcing data is coming out of another model (such as a meteorological model), most probably the input grids have a resolution that is very insufficient for Alpine3D and therefore need downscaling. If the downscaling factor is very large, we often end up with only a few points from the meteorological model that are part of the Alpine3D domain, therefore such points can be considered as "virtual stations" and spatially interpolated similarly to weather stations.
The core principles laid out in the previous section rely on the assumption that there are no lateral fluxes, which might be for some aspects too strong of an assumption. Therefore the lateral fluxes deemed relevant are introduced by other modules: