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Tomographic retrieval of cloud liquid water fields from a single scanning microwave radiometer aboard a moving platform – Part 1: Field trial results from the Wakasa Bay experiment

机译:从移动平台上的单个扫描式微波辐射计以断层图像形式检索云状液态水领域–第1部分:若狭湾实验的现场试验结果

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Tomographic methods offer great potential for retrieving three-dimensionalspatial distributions of cloud liquid water from radiometric observations bypassive microwave sensors. Fixed tomographic systems require multipleradiometers, while mobile systems can use just a single radiometer. Part 1(this paper) examines the results from a limited cloud tomography trial witha single-radiometer airborne system carried out as part of the 2003 AMSR-Evalidation campaign over Wakasa Bay of the Sea of Japan. During this trial,the Polarimetric Scanning Radiometer (PSR) and Microwave Imaging Radiometer(MIR) aboard the NASA P-3 research aircraft provided a useful dataset fortesting the cloud tomography method over a system of low-level clouds. We dotomographic retrievals with a constrained inversion algorithm using threeconfigurations: PSR, MIR, and combined PSR and MIR data. The liquid waterpaths from the PSR retrieval are consistent with those from the MIRretrieval. The retrieved cloud field based on the combined data appears to bephysically plausible and consistent with the cloud image obtained by a cloudradar. We find that some vertically-uniform clouds appear at high altitudesin the retrieved field where the radar shows clear sky. This is likely due tothe sub-optimal data collection strategy. This sets the stage for Part 2 ofthis study that aims to define optimal data collection strategies usingobservation system simulation experiments.
机译:层析成像方法为从辐射观测被动微波传感器中检索云状液态水的三维空间分布提供了巨大潜力。固定断层扫描系统需要多个辐射计,而移动系统只能使用一个辐射计。第1部分(本文)研究了2003年在日本海若狭湾进行的AMSR-Evalidation活动中使用单辐射计机载系统进行的有限云层析成像试验的结果。在此试验期间,NASA P-3研究飞机上的极化扫描辐射计(PSR)和微波成像辐射计(MIR)提供了有用的数据集,可用于测试低层云系统上的云层析成像方法。我们使用三种配置(PSR,MIR以及组合的PSR和MIR数据)使用约束反演算法进行断层摄影检索。 PSR取回的液体水径与MIRretrieval的一致。基于组合数据检索到的云场在物理上似乎是合理的,并且与cloudradar获得的云图一致。我们发现,在雷达显示晴朗天空的取回场中,一些垂直均匀的云出现在高空。这可能是由于数据收集策略欠佳所致。这为本研究的第二部分奠定了基础,该第二部分旨在通过观测系统模拟实验来定义最佳数据收集策略。

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