THE IMPACT OF DIFFERENT PHYSICAL PROCESSES AND THEIR PARAMETERIZATIONS ON FORECAST OF A HEAVY RAINFALL IN SOUTH CHINA IN ANNUALLY FIRST RAINING SEASON

被引:0
|
作者
Zhang Xu-bin [1 ,2 ]
Wan Qi-lin [1 ,2 ]
Xue Ji-shan [2 ,3 ]
Ding Wei-yu [1 ,2 ]
Li Hao-rui [1 ,2 ]
机构
[1] CMA, Guangdong Prov Key Lab Reg Numer Weather Predict, Guangzhou 510080, Guangdong, Peoples R China
[2] CMA, Inst Trop & Marine Meteorol, Guangzhou 510080, Guangdong, Peoples R China
[3] Chinese Acad Meteorol Sci, Beijing 100081, Peoples R China
基金
中国国家自然科学基金;
关键词
numerical weather prediction; heavy rainfall in South China in annually first raining season; GRAPES model; multi-physics; parameterization; ensemble prediction; CONVECTIVE ADJUSTMENT SCHEME; VERTICAL DIFFUSION; BULK PARAMETERIZATION; MESOSCALE MODEL; PRECIPITATION; RESOLUTION; IMPLEMENTATION; SIMULATIONS; SENSITIVITY; SYSTEM;
D O I
暂无
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
An ensemble prediction system based on the GRAPES model, using multi-physics, is used to discuss the influence of different physical processes in numerical models on forecast of heavy rainfall in South China in the annually first raining season (AFRS). Pattern, magnitude and area of precipitation, evolution of synoptic situation, as well as apparent heat source and apparent moisture sink between different ensemble members are comparatively analyzed. The choice of parameterization scheme for land-surface processes gives rise to the largest influence on the precipitation prediction. The influences of cumulus-convection and cloud-microphysics processes are mainly focused on heavy rainfall; the use of cumulus-convection parameterization tends to produce large-area and light rainfall. Change in parameterization schemes for land-surface and cumulus-convection processes both will cause prominent change in forecast of both dynamic and thermodynamic variables, while change in cloud-microphysics processes show primary impact on dynamic variables. Comparing simplified Arakawa-Schubert and Kain-Fritsch with Betts-Miller-Janjic schemes, SLAB with NOAH schemes, as well as both WRF single moment 6-class and NCEP 3-class with simplified explicit schemes of phase-mixed cloud and precipitation shows that the former predicts stronger low-level jets and high humidity concentration, more convective rainfall and local heavy rainfall, and have better performance in precipitation forecast. Appropriate parameterization schemes can reasonably describe the physical process related to heavy rainfall in South China in the AFRS, such as low-level convergence, latent heat release, vertical transport of heat and water vapor, thereby depicting the multi-scale interactions of low-level jet and meso-scale convective systems in heavy rainfall suitably, and improving the prediction of heavy rainfall in South China in the AFRS as a result.
引用
收藏
页码:194 / 210
页数:17
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