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

information and has been widely used for characterizing tropical convective regimes ( Masunaga et al. 2005 ), the phase of the Madden–Julian oscillation ( Lau and Wu 2010 ), and for evaluating cloud-resolving models ( Stephens et al. 2004 ; Masunaga et al. 2008 ; Matsui et al. 2009 ). If a PR H ET is found, a precipitating cloud type is assigned to the column, depending on the VIRS Tb IR and PR H ET thresholds. Warm cloud tops (Tb IR > 260 K) and shallow echo-top heights ( H ET < 4 km) are

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