Instruments and methods simulating complex snow distributions in windy environments using SnowTran-3D

被引:203
作者
Liston, Glen E. [1 ]
Haehnel, Robert B.
Sturm, Matthew
Hiemstra, Christopher A.
Berezovskaya, Svetlana
Tabler, Ronald D.
机构
[1] Colorado State Univ, Cooperat Inst Res Atmosphere, Ft Collins, CO 80523 USA
[2] USA, Cold Reg Res & Engn Lab, Hanover, NH 03755 USA
[3] USA, Cold Reg Res & Engn Lab, Ft Wainwright, AK 99703 USA
[4] Univ Alaska Fairbanks, Water & Environm Res Ctr, Fairbanks, AK 99775 USA
[5] Tabler & Associates, Niwot, CO 80544 USA
关键词
D O I
10.3189/172756507782202865
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
We present a generalized version of SnowTran-3D (version 2.0), that simulates wind-related snow distributions over the range of topographic and climatic environments found globally. This version includes three primary enhancements to the original Liston and Sturm (1998) model: (1) an improved wind sub-model, (2) a two-layer sub-model describing the spatial and temporal evolution of friction velocity that must be exceeded to transport snow (the threshold friction velocity) and (3) implementation of a three-dimensional, equilibrium-drift profile sub-model that forces SnowTran-3D snow accumulations to duplicate observed drift profiles. These three sub-models allow SnowTran-3D to simulate snow-transport processes in variable topography and different snow climates. In addition, SnowTran-3D has been coupled to a high-resolution, spatially distributed meteorological model (MicroMet) to provide more realistic atmospheric forcing data. MicroMet distributes data (precipitation, wind speed and direction, air temperature and relative humidity) obtained from meteorological stations and/or atmospheric models located within or near the simulation domain. SnowTran-3D has also been coupled to a spatially distributed energy- and mass-balance snow-evolution modeling system (SnowModel) designed for application in any landscape and climate where snow is found. SnowTran-3D is typically run using temporal increments ranging from I hour to 1 day, horizontal grid increments ranging from 1 to 100 m and time-spans ranging from individual storms to entire snow seasons.
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页码:241 / 256
页数:16
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