摘要
利用热带降雨测量卫星的微波成像仪资料,结合淮河流域试验加密观测期的阜阳地面天 气雷达雨量资料,建立了以散射指数和极化订正温度为主要参数的降水反演算法。对文 中所做反演试验与日本NASDA用微波成像仪和星载测雨雷达反演的雨强进行了比较。结果表明 ,文中所用的方法在反演陆地下垫面的降雨强度的分布和降雨区域的确定是比较成功的。
Using the matched data between the measurements of Tropical Rainfall Measure ment Mission Microwave Imager (TRMM/TMI) and those of ground based weather rad ar at Fuyang during the Intensive Observation Periods (IOPs) of GEWEX Asian Mons oon Experiment-Huaihe River Basin Experiment(GAME/HUBEX), the proper identificat ion of rain area is obtained by the dynamic cluster classification method, and a passive microwave rainfall retrieval algorithm that rain rate is a function of the scattering index and the polarization corrected temperature at 85.5 GHz is e stablished. The comparison between our retrieval test and the rainfall retrieval from the TMI and TRMM precipitation radar (PR) at the same time provided by NAS DA of Japan shows that the algorithm used in this paper is successful in retriev ing the distribution of rain rate and identifying the areas of rainfall over land.
出处
《气象学报》
CSCD
北大核心
2001年第5期591-601,共11页
Acta Meteorologica Sinica
基金
国家自然科学基金(批准号:49794030)
"高等学校骨干教师资助计划"。