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熱圏下部を周期的に加熱した場合の風系と温度変化について
http://hdl.handle.net/10069/16473
http://hdl.handle.net/10069/1647345532805-7ed1-4f1f-bc05-6b109dfdaa4a
名前 / ファイル | ライセンス | アクション |
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kyoyoS12_00_02_t.pdf (373.6 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 | 熱圏下部を周期的に加熱した場合の風系と温度変化について | |||||
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 and the temperature variation in the case of heating the lower part of the Thermosphere periodically | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | A wind system and pressure and temperature oscillations are studied when the lower part of the Thermosphere (around 90-110 km) is heated periodically. The obtained results are follows: (1) the wind components and all oscillations predominate in and above the heating layer, (2) only one node is formed in the heating layer in the case of the westerly, northerly and pressure oscillation, and therefore, these phases have a jump of 180 in the same layer, (3) in the case of the vertical wind and the temperature oscillation, no node is formed. | |||||
書誌情報 |
長崎大学教養部紀要. 自然科学 巻 12, p. 7-13, 発行日 1971-12-25 |
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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. 1971, 12, p.7-13 |