A two-moment bulk microphysics coupled with a mesoscale model WRF: Model description and first results

被引:17
|
作者
Gao Wenhua [1 ]
Zhao Fengsheng [1 ]
Hu Zhijin [2 ]
Feng Xuan [1 ]
机构
[1] China Meteorol Adm, Natl Satellite Meteorol Ctr, Beijing 100081, Peoples R China
[2] China Meteorol Adm, Chinese Acad Meteorol Sci, Beijing 100081, Peoples R China
基金
中国国家自然科学基金;
关键词
droplet activation; two-moment bulk microphysics; WRF; coupling; CLOUD CONDENSATION NUCLEI; GENERAL-CIRCULATION MODEL; MIXED-PHASE CLOUDS; PART I; SENSITIVITY EXPERIMENTS; CONVECTIVE STORMS; ICE-NUCLEATION; CLIMATE MODELS; LIQUID WATER; PARAMETERIZATION;
D O I
10.1007/s00376-010-0087-z
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The Chinese Academy of Meteorological Sciences (CAMS) two-moment bulk microphysics scheme was adopted in this study to investigate the representation of cloud and precipitation processes under different environmental conditions. The scheme predicts the mixing ratio of water vapor as well as the mixing ratios and number concentrations of cloud droplets, rain, ice, snow, and graupel. A new parameterization approach to simulate heterogeneous droplet activation was developed in this scheme. Furthermore, the improved CAMS scheme was coupled with the Weather Research and Forecasting model (WRF v3.1), which made it possible to simulate the microphysics of clouds and precipitation as well as the cloud-aerosol interactions in selected atmospheric condition. The rain event occurring on 27-28 December 2008 in eastern China was simulated using the CAMS scheme and three sophisticated microphysics schemes in the WRF model. Results showed that the simulated 36-h accumulated precipitations were generally agreed with observation data, and the CAMS scheme performed well in the southern area of the nested domain. The radar reflectivity, the averaged precipitation intensity, and the hydrometeor mixing ratios simulated by the CAMS scheme were generally consistent with those from other microphysics schemes. The hydrometeor number concentrations simulated by the CAMS scheme were also close to the experiential values in stratus clouds. The model results suggest that the CAMS scheme performs reasonably well in describing the microphysics of clouds and precipitation in the mesoscale WRF model.
引用
收藏
页码:1184 / 1200
页数:17
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