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用TRMM资料研究江淮、华南降水的微波特性
引用本文:吴庆梅,程明虎,苗春生.用TRMM资料研究江淮、华南降水的微波特性[J].应用气象学报,2003,14(2):206-214.
作者姓名:吴庆梅  程明虎  苗春生
作者单位:1.北京市气象局, 北京 100089
基金项目:国家重点基础研究发展规划项目 (G19980 4 0 90 9),优秀归国留学人员重点基金共同资助
摘    要:热带测雨卫星TRMM (Tropical Rainfall Measuring Mission) 于1997年11月发射成功, 其首次携带了空载雷达, 有关资料已在网上对公众发布。利用热带测雨卫星上的微波成像仪TMI (TRMM Microw ave Imager) 资料以及其和测雨雷达TRMM/PR (Precipitation Radar) 资料联合反演的地面瞬时降水产品, 采用散射指数 (Is) 法从理论上探讨了我国江淮、华南降水尤其是暴雨的微波特性, 其中Is表达式通过江淮、华南晴空TMI资料统计回归得到。以联合反演的地面瞬时降水产品为真值, 用面积相当法对14个降水个例求Is降水阈值, 研究了阈值和降水面积以及85.5 GHz垂直通道最低亮温的关系, 并寻求了Is和降水的相关特征。研究表明:Is降水阈值随降水面积的增大或85.5 GHz垂直通道最低亮温的降低有增高的趋势; Is与强对流性降水瞬时雨强对应很好, Is≥60 K是一个好的暴雨指标。最后进行了初步的雨强反演试验研究, 由于TMI资料分辨率的提高以及时空配合较好的真值, 反演的地面瞬时降水与真值相关效果大大提高。

关 键 词:TMI    散射指数    降水阈值    瞬时雨强
收稿时间:2002-01-04
修稿时间:2002年1月4日

Study of Microwave Characteristics of Rainfall over South China and Yangtze River Basin Using TRMM Data
Wu Qingmei,Cheng Minghu,Miao Chunsheng.Study of Microwave Characteristics of Rainfall over South China and Yangtze River Basin Using TRMM Data[J].Quarterly Journal of Applied Meteorology,2003,14(2):206-214.
Authors:Wu Qingmei  Cheng Minghu  Miao Chunsheng
Affiliation:1.Beijing Meteorological Bureau, Beijing 1000892.Chinese Academy of Meteorology Sciences, Beijing 1000813.Nanjing I nstitute of Meteorology, Nanjing 210044
Abstract:TRMM (Tropical Rainfall Measurement Mission) was launched in December 1997, which carried a space radar for the first time and the related data have been made available to the public users since June 1998.The microwave characteristics of rainfall over South China and the Yang tze river basin are investigated by using TMI (TRMM Microwave Imager) data and TRMM-derived precipitation products through Is (Scattering Index) algorithm.The expression of the Isis regressed by the TMI data on sunny days.For 14 rainfall cases, the relationship between the Isprecipitation threshold obtained through the "area equal" method and the precipitation area and the coldest top temperature of 85.5 GHz vertical channel is investigated.At the same time, the correlation between Isand surface instantaneous rain intensity is studied.The result shows that the Isthreshold has the increasing tendency when the precipitation area increases or the top temperature decreases, and Is≥60 K is a good index of rainstorm.The instantaneous rain intensity is retrieved, and it is found that Iscan be used to retrieve rain intensity better because of the improvement of data resolution and the temporal and spatial consistency of the data.
Keywords:TMI  Scattering index  Threshold  Instantaneous rain intensity
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