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Toshi Matsui, Jiun-Dar Chern, Wei-Kuo Tao, Stephen Lang, Masaki Satoh, Tempei Hashino, and Takuji Kubota

returned echo is sensitive to precipitating liquid and frozen particles. VIRS Tb IR is sensitive to cloud droplets or ice crystal emission so that it represents the cloud-top temperature of optically thick clouds. TMI Tb 85 depression (i.e., scattering) is correlated with the amount of relatively small as well as large precipitation-sized ice particles, which provide additional information in the convective system [section 3c in Matsui et al. (2009) ]. To construct the collocated signal database

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