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Measurements and implications for combined radar-passive microwaverainfall profiling techniques

机译:雷达无源微波雨量分析技术组合的测量和意义

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An upcoming NASA satellite platform, the Tropical RainfallnMeasuring Mission (TRMM), represents the first opportunity tonincorporate both multifrequency passive microwave and active radarnmeasurements in its retrieval algorithms. The TRMM microwave imagern(TMI) includes many of the same passive channels as the current SpecialnSensor Microwave Imager (SSMI), with the addition of a 10.7 GHz channel.nThe 14 GHz incoherent precipitation radar (PR) scans an across-tracknswath width about one-third the width of the forward-view conical TMInscan. Therefore, the radar data arrives about a minute after the TMInscan, and the PR and TMI beams view significantly different profiles innthe atmosphere for a given on-Earth pixel location. During the 1992-1993nTOGA-COARE experiment in the western Pacific Ocean, a DC-8-basednprecipitation radar and an ER-a-based 4-channel microwave radiometerngathered data over a multitude of precipitating storm regions includingnthe forming and mature stages of a tropical cyclone. Example imagery andnvertical radar profiles are presented. These data are currently beingnused by the authors for vertical profiling algorithms which exploit theninformation contained in both the radar and radiometer. The radar datanprovide clues to the underlying cloud vertical structure that can benused to mitigate ambiguities in profile-based retrieval algorithms thatnrely upon the passive TB alone
机译:即将到来的NASA卫星平台热带降雨测量任务(TRMM)代表了将多频无源微波和有源雷达测量技术纳入其检索算法的第一个机会。 TRMM微波成像(TMI)包括许多与当前SpecialnSensor微波成像仪(SSMI)相同的无源通道,并增加了10.7 GHz通道。n14 GHz非相干降水雷达(PR)扫描整个跨径道宽度约一个-正视圆锥形TMInscan的宽度的三分之一。因此,雷达数据到达TMInscan大约一分钟后,对于给定的地球上像素位置,PR和TMI光束在大气中观察到明显不同的剖面。在1992年至1993年的nTOGA-COARE实验在西太平洋进行期间,基于DC-8的降水雷达和基于ER-a的4通道微波辐射计收集了包括热带气旋形成和成熟阶段在内的众多降水风暴区域的数据。给出了示例图像和垂直雷达剖面图。作者目前正在为垂直分析算法使用这些数据,该算法利用了雷达和辐射计中包含的信息。雷达数据提供了潜在的云垂直结构的线索,这些线索可用来减轻仅基于被动T B 的基于配置文件的检索算法中的歧义

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