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作 者:Li Li Yuanjing Zhu Bolin Zhao
机构地区:[1]Peking Univ, State Key Lab Severe Storm Res, Dept Geophys, Beijing 100871, Peoples R China
出 处:《Chinese Science Bulletin》1998年第22期1913-1917,共5页
基 金:theNationalNaturalScienceFoundationofChina(GrantNo .4 9794 0 30 );alsobyScienceResearchFoundationofShanghaiNormalUniversityforteacherswithPh .D
摘 要:Composite microwave index (CMI) method is used with the satellite SSM/I data to retrieve summer rainfall rate over 96°E-127°E, 17°N-44°N. The results of verification are : the root_of_mean_square error is 0.9 mm/h in the actual rain rate range from 2 to 2.9 mm/h; 1.6 mm/h in that from 3 to 5 mm/h and the maximum rms error is 4.2 mm/h in that from 5.1 to 50 mm/h. Case study shows the decision tree and CMI method presented in the note are effective to the rainfall recognition and rain rate retrieval over land of East China.Composite microwave index (CMI) method is used with the satellite SSM/I data to retrieve summer rainfall rate over 96°E–127°E, 17°N–44°N. The results of verification are: the root-of-mean-square error is 0.9 mm/ h in the actual rain rate range from 2 to 2.9 mm/ h; 1.6 mm/h in that from 3 to 5 mm/h and the maximum rms error is 4.2 mm/h in that from 5.1 to 50 mm/h. Case study shows the decision tree and CMI method presented in the note are effective to the rainfall recognition and rain rate retrieval over land of East China.
关 键 词:satellite microwave REMOTE sensing RAINFALL RETRIEVAL OVER land.
分 类 号:P414.9[天文地球—大气科学及气象学]
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