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Atsushi Hamada and Yukari N. Takayabu

understanding of such processes by producing measurements from its non-sun-synchronous orbit. Another important purpose of the GPM DPR, in conjunction with the TRMM PR, is to produce three-dimensional distributions of latent heating ( Simpson et al. 1996 ; Takayabu 2002 ; Shige et al. 2004 , 2007 ; Tao et al. 2010 ). Even in the tropics, there is still no unified view with regard to the diabatic heating structure, because of the large discrepancies among current global reanalysis datasets and estimates

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