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タイトル: 上部オゾン層と下部対流圏を加熱した場合の風系について
その他のタイトル: The Wind System in the Case of Heating the Upper Part of the Ozonosphere and the Lower One of the Troposphere
著者: 松島, 晟
著者(別表記) : Matsushima, A.
発行日: 1970年12月25日
引用: 長崎大学教養部紀要. 自然科学. 1970, 11, p.7-13
抄録: In this paper some physical quantities, especially wind components are studied when the upper part of the ozonosphere and the lower one of the troposphere are heated simultaneously. The result is as follows: so far as the total heat given to the lower part of the troposphere is up to approximately three times more than the total heat given to the upper part of the ozonosphere; (1) the physical quantities in the troposphere are much influenced, but those in the mesosphere are little influenced, by this tropospheric heating, (2) the northerly wind component has two nodes in the region below 25 km, (3) at least in the troposphere, the more the total heat given in the troposphere is, the stronger the vertical wind component becomes.
URI: http://hdl.handle.net/10069/16468
ISSN: 02871319
資料タイプ: Departmental Bulletin Paper
原稿種類: publisher

引用URI : http://hdl.handle.net/10069/16468



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