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CAMS三维对流云催化模式的改进及个例模拟
引用本文:李淑日,胡志晋,王广河.CAMS三维对流云催化模式的改进及个例模拟[J].应用气象学报,2003,14(Z1):78-91.
作者姓名:李淑日  胡志晋  王广河
作者单位:李淑日(中国气象科学研究院,北京,100081)       胡志晋(中国气象科学研究院,北京,100081)       王广河(中国气象科学研究院,北京,100081)
基金项目:本研究由国家重点科技攻关项目(96-908-07)、(2001BA610A-06-01)共同资助.
摘    要:该文对CAMS原有的三维对流云模式(2000版)进行了改进,引入雪晶的比水量和数浓度作为预报变量,加进与雪晶有关的11种微物理过程,从而使模式的微物理过程更加完善,使其能更好的模拟对流云降水过程.通过对1996年北京雹云个例模拟,发现模式模拟云的多单体结构、回波顶高、强中心位置与雷达观测比较一致,并能很好的解释地面雹块结构的形成原因.对改进前后的模式计算结果进行对比分析发现改进前后动力场变化不大,主要是微物理过程产生的影响,同时该文还对改进后的模式进行了AgI催化模拟试验.

关 键 词:对流云  雪晶  AgI催化
修稿时间:2002年1月15日

IMPROVEMENT AND SIMULATION OF THREE-DIMENSION CONVECTIVE CLOUD SEEDING MODEL OF CAMS
Li Shuri,Hu Zhijin,Wang Guanghe.IMPROVEMENT AND SIMULATION OF THREE-DIMENSION CONVECTIVE CLOUD SEEDING MODEL OF CAMS[J].Quarterly Journal of Applied Meteorology,2003,14(Z1):78-91.
Authors:Li Shuri  Hu Zhijin  Wang Guanghe
Abstract:The CAMS 3 D convective cloud model was improved by adding snow as a new kind of hydrometeor to describe the micro physics processes better, so to simulate the convective cloud precipitation processes. The simulation results of a hail cloud case in Beijing in 1996 show that the simulated multi cell structure, echo depth and strong echo center of the clouds are similar to the observation. It explains the cause of the structure of hailstones. The comparison between the results of the improved model and the primary model show that the difference is small in the dynamical fields, and the main reason leading to the enhanced precipitation is the effect of the microphysical processes. An AgI seeding experiment was also conducted with the improved model.
Keywords:Convective cloud  Snow  AgI seeding
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