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The Cryosphere An interactive open-access journal of the European Geosciences Union
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Volume 2, issue 1
The Cryosphere, 2, 53–66, 2008
© Author(s) 2008. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 2, 53–66, 2008
© Author(s) 2008. This work is distributed under
the Creative Commons Attribution 3.0 License.

  23 May 2008

23 May 2008

Is snow sublimation important in the alpine water balance?

U. Strasser1, M. Bernhardt1, M. Weber2, G. E. Liston3, and W. Mauser1 U. Strasser et al.
  • 1Department of Geography, Ludwig-Maximilians University (LMU), Luisenstr. 37, 80333 Munich, Germany
  • 2Comm. for Glaciology, Bavarian Academy of Sciences and Humanities, Alfons-Goppel-Str. 11, 80539 Munich, Germany
  • 3Cooperative Institute for Research in the Atmosphere, Colorado State University, Fort Collins, Colorado 80523, USA

Abstract. In alpine terrain, snow sublimation represents an important component of the winter moisture budget, representing a proportion of precipitation which does not contribute to melt. To quantify its amount we analyze the spatial pattern of snow sublimation at the ground, from a canopy and from turbulent suspension during wind-induced snow transport for a high alpine area in the Berchtesgaden National Park (Germany), and we discuss the efficiency of these processes with respect to seasonal snowfall. Therefore, we utilized interpolated meteorological recordings from a network of automatic stations, and a distributed simulation framework comprising validated, physically based models. The applied simulation tools were: a detailed model for shortwave and longwave radiative fluxes, a mass and energy balance model for the ground snow cover, a model for the microclimatic conditions within a forest canopy and related snow-vegetation interactions including snow sublimation from the surface of the trees, and a model for the simulation of wind-induced snow transport and related sublimation from suspended snow particles. For each of the sublimation processes, mass rates were quantified and aggregated over an entire winter season. Sublimation from the ground and from most canopy types are spatially relatively homogeneous and sum up to about 100 mm of snow water equivalent (SWE) over the winter period. Accumulated seasonal sublimation due to turbulent suspension is small in the valley areas, but can locally, at very wind-exposed mountain ridges, add up to more than 1000 mm of SWE. The fraction of these sublimation losses of winter snowfall is between 10 and 90%.

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