A PREDICTION MODEL FOR SNOWMELT, SNOW SURFACE-TEMPERATURE AND FREEZING DEPTH USING A HEAT-BALANCE METHOD

被引:0
|
作者
KONDO, J
YAMAZAKI, T
机构
来源
JOURNAL OF APPLIED METEOROLOGY | 1990年 / 29卷 / 05期
关键词
D O I
10.1175/1520-0450(1990)029<0375:APMFSS>2.0.CO;2
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
This model takes into account both the heat balance at the snow surface and that of the entire snow cover and simultaneously predicts the snow surface temperature and freezing depth. Observed or estimated incident radiation data are required for operation of the model. Calculated amounts of snowmelt and snow surface temperatures were in agreement with those observed. Dependency of snowmelt on several parameters including maximum liquid water content, thermal conductivity and albedo of the snow was examined. It was found that as liquid water content or thermal conductivity increases, snowmelt decreases. Albedo is very influential in evaluating snowmelt. -from Authors
引用
收藏
页码:375 / 384
页数:10
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