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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
http://hdl.handle.net/10069/16468
http://hdl.handle.net/10069/16468a5f01066-2bde-4ffb-9104-92ed256e95e5
名前 / ファイル | ライセンス | アクション |
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kyoyoS11_00_02_t.pdf (268.1 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2008-04-11 | |||||
タイトル | ||||||
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 | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
著者 |
松島, 晟
× 松島, 晟 |
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著者別名 | ||||||
姓名 | Matsushima, A. | |||||
その他のタイトル | ||||||
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 | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | 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. | |||||
書誌情報 |
長崎大学教養部紀要. 自然科学 巻 11, p. 7-13, 発行日 1970-12-25 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 02871319 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00178360 | |||||
著者版フラグ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
sortkey | ||||||
P00007-P00013 | ||||||
引用 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 長崎大学教養部紀要. 自然科学. 1970, 11, p.7-13 |