著者

千葉 修 小林 文明 金田 昌樹

出版者

高知大学大学院黒潮圏海洋科学研究科

雑誌

黒潮圏科学 = Kuroshio Science (ISSN:1882823X)

巻号頁・発行日

vol.5, no.2, pp.169-174, 2012-03-25

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To survey the weather at the time of the 2011 off the Pacific coast of Tohoku Earthquake occurred on 11 March,2011, meteorological data were used for analysis.In particular, we examined the influence that the massive tsunami that came in the Sendai plains gave the atmosphere, based on AMEDAS data of the East Japan in addition to the weather data at 10-second intervalsof the Sendai district meteorological observatory. As a result, the southeastern wind blown in the coast of inland (Natori, Watari) from Sendai Bay is more likely to bewind with the tsunamis.