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Hironari Kanamori, Tomo’omi Kumagai, Hatsuki Fujinami, Tetsuya Hiyama, and Tetsuzo Yasunari

Yasunari 2008 ). It is interesting to note that the strength of the seasonality of both P and C for all domains in Fig. 4 depends on the combined effects of large-scale circulations, for example, the positions of both the ITCZ and the SPCZ, and the northeasterly winter monsoon. Fig . 4. Climatological (1998–2012) mean monthly precipitation P , moisture flux convergence C , temporal change in precipitable water content W (mm day −1 ), and LWUR (%) over (a) BOL, (b) NGL, (c) BOC, (d) NGC, and

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