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Takuya Kawabata, Tohru Kuroda, Hiromu Seko, and Kazuo Saito

rectangle on a surface weather map ( Fig. 6 ), covered the Kanto plain. A stationary front extended from north of Kyushu to the northern part of Japan. Typhoon 0514 (NABI) can be seen over the sea east of Okinawa, but the Kanto plain is 1500 km away and was not directly affected by the typhoon. Since there were no distinct disturbances around the Kanto plain, meteorological forcing larger than meso- α – β scale was weak. Fig . 6. Surface weather map on 2100 JST 4 Sep 2005. A small rectangular region

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