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Conclusion (1 of 2)• Tokai-storm DAD characteristics was quantitativelyexplained. It illustrates that a)Tokai storm overallwas smaller than Japan’s largest level, b) DD –relations were the closest to the Japan’s maximumin 6-12 hours duration, c)regarding the DADcharacteristics,areal rainfall decreasing rate witharea were smaller than the Japan’s maximum DAD.The last point suggests the necessity to re-assess theJapan’s maximum DAD enveloping curves with theTokai rainstorm data.

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