The purpose of this paper is to clarify the regionality of rainfall fluctuation in and around Japan (Fig. 1) in July. Using the data of monthly precipitation during 1951-1980, “cluster analysis” based on similarity of interannual fluctuations was applied (Fig. 2). The area was divided into five regions (A-E) which were distributed from north to south (Fig. 3). Fluctuations of areal mean rainfall of the regions were compared with each other from the the viewpoint of anomaly.
A change of interrelation on rainfall fluctuation among the regions was found at the latter half of 1960's (Figs. 4 and 5), which means a turning point as to geographical pattern in rainfall fluctuation.
Characteristics of year-to-year vasiation of anomaly distribution during 1951-1971, the former period, was northward or southward gradual movement of the areas with +sign and -sign anomaly (Fig. 7, Table 1).
During the latter period (1967-1980), the following two patterns of anomaly distribution appeared frequently (Table 2), being connected to the appearence of fronts at the 850mb level (Fig. 6).
(I) +area: Honshu, Shikoku and Kyushu.
-area: Over Hokkaidou and Ryukyu Islands.
(II) +area: Over the sea of Okhotsk and Ryukyu Islands.
-area: From Hokkaidou to Kyushu.
From these facts, it is found that the two periods are different each other on the variation mode of rainfall distribution in and around Japan in July.
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