Abstract
The relation between the rainfall of various districts and the typhoon is settled by the position and the track of typhoon.
The rainfall of various districts as a rule when the typhoon exists southwards from the line of the 28th degree of the north latitude.
The rainfall of Mitsuse is nearly doubles of Saga as Fig. 1 when the typhoon passes the west or north side of Saga.
The rainfall of Mitsuse is about eleven fold of Saga as Fig. 2 when the typhhoon lands in the southern end of Kyushu and then progresses to north-north-eastwards or the typhoon passes the east of Miyazaki and then progresses to northwards.
But the rainfall of Mitsuse is only thrice when the typhoon lands in the southern end of Kyushu and then progresses to northwards.
