摘要
本文利用 NCAR/PSU联合研制的中尺度天气数值模式 MMS,对长 江中下游地区在1996年6月下旬至7月中旬发生的暴雨过程,以国家气象中心业 务运行的全球谱模式T63的分析场作为初值和侧边界条件,进行了一系列的数值 预报试验。结果表明,该模式较好地预报了与实况相近的降雨区的位置,但对暴雨 的中心落点和强度,其预报结果与实测有一定程度的偏差。如果模式提前12小时 开始积分,则可在一定程度上克服模式中凝结降水的旋转加强问题,使预报的降水 强度等有明显的改善。
In this paper a series of experiments of the heavy rain processes occurring in the period from the third dekad in June to the second dekad in July of 1996 are made by using the NCAR/PSU mesoscale numerical weather model MM5. The analysis data of the global spectral model T63 at National Meteorological Center in China are used as initial and lateral boundary conditions necessary to drive the model runs. The results show that the model can predict the location of rainfall area, which is much close to the observation. However, there are some departures for location and density of heavy rain. If the model begins 12 hours earli- er,the spin-up problem of condensation rainfall in the model would been got over and pre- dicted rainfall density would become more reasonable.
出处
《气象科学》
CSCD
北大核心
2001年第1期19-27,共9页
Journal of the Meteorological Sciences
基金
国家重点基础研究项目!(G1998040908)资助
博士荃全!(98028402)项目资助
关键词
长江中下游
暴雨
数值预报试验
降水强度
过程分析
Middle and lower of Changjiang River Vellay Heavy rain numerical pre- diction experiments