Evaluation of snow-surface energy balance models in alpine terrain

被引:38
作者
Fierz, C
Riber, P
Adams, EE
Curran, AR
Föhn, PMB
Lehning, M
Plüss, C
机构
[1] WSL, Swiss Fed Inst Snow & Avalanche Res, SLF, CH-7260 Davos, Switzerland
[2] Ctr Natl Rech Meteorol Meteo France, F-31057 Toulouse, France
[3] Montana State Univ, Dept Civil Engn, Bozeman, MT 59717 USA
[4] ThermoAnal Inc, Calumet, MI 49913 USA
关键词
snow; alpine snow cover; snow cover energy balance; topographic effects; snow melt; snow cover simulation;
D O I
10.1016/S0022-1694(03)00255-5
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The increasing complexity of snow-cover models demands high-quality forcing data. In complex alpine terrain, both short and long wave incoming radiation components are expected to be influenced by small-scale topographic effects, i.e. shading and multiple scattering as well as long-wave irradiance from the surroundings. Not only should the latter be included in distributed energy balance models, but, because of their increasing resolution, also in meteorological models of the next generation. The energy balance at the snow-cover surface is calculated by means of different distributed energy balance models over a region of a few square kilometres. the spatial resolution being 25 m. The models include topographical effects on the radiation components of the energy balance. The region of interest is located in the Eastern Swiss Alps, around study sites of the Swiss Federal Institute for Snow and Avalanche Research SLF, Davos. The primary forcing data are taken from automatic weather stations located within the study area. To assess performance and differences of the models, two approaches are taken. First, model outputs are compared to measurements of both incoming radiation and snow surface temperature measured at automatic weather stations located on either level or inclined terrain within the region. Second, the models are used to calculate snowmelt at the beginning of the ablation period. The results are compared with changes of the snow water equivalent as measured in various spots of the modelled region, including all aspects on one elevation range. In view of the above comparison, the necessity to include small-scale topographic influences on the energy balance at the snow-cover surface as well as to consider snow surface properties and internal processes within the snow cover will be discussed. The possible implications for hydrological and meteorological models of the next generation will be addressed too. (C) 2003 Elsevier B.V. All rights reserved.
引用
收藏
页码:76 / 94
页数:19
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