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Related Projects

Publications

  • Lehning et al.: ALPINE3D: A detailed model of mountain surface processes and its application to snow hydrology. Link
  • Kuonen, P. et al.: POP-C++ and Alpine3D: petition for a new HPC approach. Link
  • Bavay et al.: Simulations of future snow cover and discharge in Alpine headwater catchments. Link
  • Raderschall et al.: Fine scale modelling of the boundary layer wind field over steep topography. Link

Alpine3D

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.

Alpine3D    

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:

  • the EBalance module computes the radiation fields, taking into account atmospheric cloudiness, topographic shading effects and reflections by the surrounding terrain.
  • the SnowDrift module that simulates the transport of snow by the wind. It performs a 3D simulation of the saltation, suspension and diffusion processes.
  • the runoff module that collects the precipitation and/or melt water at each pixel to transfer it to an hydrological routing module