摘要
为研究边界层过程中地表阻曳系数对短期数值预报(特别是降水)的影响,利用复杂地形条件下有限区域数值预报模式,根据青藏高原及其北侧部分地区已有的观测结果,改变了不同地区地面阻曳系数及其组合,设计出4种不同的数值试验方案,对1991年6月11—15日的一次典型江淮梅雨天气过程进行了24—96h数值预报试验。结果表明:(1)地表阻曳系数对雨量中心强度的短期预报有一定影响;(2)4个方案中以修改了青藏高原及其北侧地区阻曳系数值的方案2更好些;(3)随积分时间延长。
In this paper,the limite-area numerical weather forecasting model suitable for complex topography and the observation data over Tibetan Plateau and part area of its north-side are used to study the influences of surface dray coefficients in boundary process on numerical weather forecasting ( especially precipitation forecasting ) Firstly,dray coefficients of different underlying surface are altered and combined Secondly,4 groups of different numerical experiment schemes are designed At last,24 96h numerical forecasting experiments about a typical Jianghuai Meiyu heavy rain weather process during 11 15 June,1991 have been carried out The results show: (1) Surface dray coefficients has some influences on short-range forecasting of center intensity of rainfall (2) Among 4 schemes,scheme 2,in which the drag coefficients over Tibetan Plateau and part area of its north-side are modified,has a better result (3) With integration time prolonging,the influences about boundary process on rainfall and weather situation are more notable
出处
《高原气象》
CSCD
北大核心
1995年第4期434-442,共9页
Plateau Meteorology
基金
国家八.五科技攻关项目85-906-46(08-06)
中科院重大项目KY85-10-344子专题资助
关键词
边界层过程
阻曳系数
暴雨
数值天气预报
s Boundary process Drag coefficients Heavy rain Numerical forecasting experiment