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海の潮汐について
http://hdl.handle.net/10069/16622
http://hdl.handle.net/10069/16622837fdc89-5ff2-44e6-ae7e-dbcb3b98890b
名前 / ファイル | ライセンス | アクション |
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kyoyoS32_01_01_t.pdf (188.9 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2008-04-14 | |||||
タイトル | ||||||
タイトル | 海の潮汐について | |||||
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 |
古賀, 雅夫
× 古賀, 雅夫× 松島, 晟× 武政, 剛弘 |
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著者別名 | ||||||
姓名 | Koga, Masao | |||||
著者別名 | ||||||
姓名 | Matsushima, Akira | |||||
著者別名 | ||||||
姓名 | Takemasa, Takehiro | |||||
その他のタイトル | ||||||
その他のタイトル | On The Tide of The Ocean | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The tide of the idealized global ocean with a uniform depth is studied in terms of the resonance theory. The following results are found: 1. The period of the zonal free oscillations varies with the integer n which represents the oscillation mode in the north-south direction and the depth h of the ocean. In other words, the period becomes shorter as n becomes larger or the depth h becomes deeper. 2. In the case of oscillations other than zonal ones, the period is expressed explicitly by the depth h. | |||||
書誌情報 |
長崎大学教養部紀要. 自然科学篇 巻 32, 号 1, p. 1-5, 発行日 1991-07-31 |
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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 | AN10352293 | |||||
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 | ||||||
P00001-P00005 | ||||||
引用 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 長崎大学教養部紀要. 自然科学篇. 1991, 32(1), p.1-5 |