ATSC 5210 Kyoko Taniguchi Warm
نویسنده
چکیده
The warm rain process refers to the precipitation formation from warm clouds, which involves no ice phase through the whole process. Therefore, the entire cloud is below the freezing height all the time, unless cloud droplets are supercooled, so they remain in the liquid phase below the freezing temperature. This process is commonly observed in, but not limited to, tropical regions because of high moisture content. In fact, such a process has been reported in various places (Fig. 1).
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