A distributed snow-evolution modeling system (SnowModel)

被引:390
作者
Liston, Glen E. [1 ]
Elder, Kelly
机构
[1] Colorado State Univ, Cooperat Inst Res Atmosphere, Ft Collins, CO 80523 USA
[2] US Forest Serv, USDA, Rocky Mt Res Stn, Ft Collins, CO USA
关键词
D O I
10.1175/JHM548.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
SnowModel is a spatially distributed snow-evolution modeling system designed for application in landscapes, climates, and conditions where snow occurs. It is an aggregation of four submodels: MicroMet defines meteorological forcing conditions, EnBal calculates surface energy exchanges, SnowPack simulates snow depth and water-equivalent evolution, and SnowTran-3D accounts for snow redistribution by wind. Since each of these submodels was originally developed and tested for nonforested conditions, details describing modifications made to the submodels for forested areas are provided. SnowModel was created to run on grid increments of 1 to 200 m and temporal increments of 10 min to 1 day. It can also be applied using much larger grid increments, if the inherent loss in high-resolution (subgrid) information is acceptable. Simulated processes include snow accumulation; blowing-snow redistribution and sublimation; forest canopy interception, unloading, and sublimation; snow-density evolution; and snowpack melt. Conceptually, SnowModel includes the first-order physics required to simulate snow evolution within each of the global snow classes (i.e., ice, tundra, taiga, alpine/mountain, prairie, maritime, and ephemeral). The required model inputs are 1) temporally varying fields of precipitation, wind speed and direction, air temperature, and relative humidity obtained from meteorological stations and/or an atmospheric model located within or near the simulation domain; and 2) spatially distributed fields of topography and vegetation type. SnowModel's ability to simulate seasonal snow evolution was compared against observations in both forested and nonforested landscapes. The model closely reproduced observed snow-water-equivalent distribution, time evolution, and interannual variability patterns.
引用
收藏
页码:1259 / 1276
页数:18
相关论文
共 132 条
  • [31] OBSERVED IMPACT OF SNOW COVER ON THE HEAT-BALANCE AND THE RISE OF CONTINENTAL SPRING TEMPERATURES
    GROISMAN, PY
    KARL, TR
    KNIGHT, RW
    [J]. SCIENCE, 1994, 263 (5144) : 198 - 200
  • [32] Solar radiation transmission through conifer canopies
    Hardy, JP
    Melloh, R
    Koenig, G
    Marks, D
    Winstral, A
    Pomeroy, JW
    Link, T
    [J]. AGRICULTURAL AND FOREST METEOROLOGY, 2004, 126 (3-4) : 257 - 270
  • [33] HARDY JR, 2004, SUB CANOPY ENERGETIC
  • [34] Hasholt B, 2003, NORD HYDROL, V34, P1
  • [35] Hedstrom NR, 1998, HYDROL PROCESS, V12, P1611, DOI 10.1002/(SICI)1099-1085(199808/09)12:10/11&lt
  • [36] 1611::AID-HYP684&gt
  • [37] 3.0.CO
  • [38] 2-4
  • [39] Hellström RÅ, 2000, HYDROL PROCESS, V14, P3239, DOI 10.1002/1099-1085(20001230)14:18&lt
  • [40] 3239::AID-HYP201&gt