A Parameterization of the Microphysical Processes Forming Many Types of Winter Precipitation

被引:54
|
作者
Theriault, Julie M. [1 ]
Stewart, Ronald E. [1 ]
机构
[1] McGill Univ, Dept Atmospher & Ocean Sci, Montreal, PQ H3A 2K6, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
MICROSCALE STRUCTURE; FRONTAL RAINBANDS; ICE CRYSTALS; PART I; STORM; CAPACITANCE; SNOWFLAKES; MESOSCALE; SCHEME; CLOUD;
D O I
10.1175/2009JAS3224.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Several types of precipitation, such as freezing rain, ice pellets, and wet snow, are commonly observed during winter storms. The objective of this study is to better understand the formation of these winter precipitation types. To address this issue, detailed melting and refreezing of precipitation was added onto an existing bulk microphysics scheme. These modifications allow the formation of mixed-phase particles and these particles in turn lead to, or affect, the formation of many of the other types of precipitation. The precipitation type characteristics, such as the mass content, liquid fraction, and threshold diameters formed during a storm over St John's, Newfoundland, Canada, are studied and compared with observations. Many of these features were reproduced by the model. Sensitivity experiments with the model were carried out to examine the dependence of precipitation characteristics in this event on thresholds of particle evolution in the new parameterization.
引用
收藏
页码:1492 / 1508
页数:17
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