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1988年夏期 西部熱帯太平洋に於ける海況
http://hdl.handle.net/10232/13373
http://hdl.handle.net/10232/13373e83185cb-61b3-4ad5-9869-92fd0d4f31a9
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
AN00040498_v37_p97-109.pdf (1.3 MB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2012-05-07 | |||||
| タイトル | ||||||
| タイトル | Oceanic Conditions in the Western Tropical Pacific in the Summer of 1988 | |||||
| タイトル言語 | en | |||||
| タイトル | ||||||
| タイトル | 1988年夏期 西部熱帯太平洋に於ける海況 | |||||
| タイトル言語 | ja | |||||
| 著者 |
湯脇, 泰隆
× 湯脇, 泰隆× 西, 徹× 益滿, 侃× 東, 政能 |
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| 言語 | ||||||
| 言語 | eng | |||||
| キーワード | ||||||
| 主題言語 | en | |||||
| 主題Scheme | Other | |||||
| 主題 | Oceanic condition | |||||
| キーワード | ||||||
| 主題言語 | en | |||||
| 主題Scheme | Other | |||||
| 主題 | Western Tropical Pacific | |||||
| キーワード | ||||||
| 主題言語 | en | |||||
| 主題Scheme | Other | |||||
| 主題 | Equatorial Current | |||||
| 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 | |||||
| アクセス権 | ||||||
| アクセス権 | open access | |||||
| アクセス権URI | http://purl.org/coar/access_right/c_abf2 | |||||
| 要約 | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | Oceanographic observations using a CTD system were made in the Western Tropical Pacific in the summer of 1988. The first oceanographic section was made along 133°E from 20°N to 10°N from June 13-18th, and the second one from 09°N, 138°E to 00°, 149°E from June 25-28th. The warm surface water having a value of above 29°C was presented over the whole sea surface. The thermocline with the maximum vertical gradient having a value of 0.17°C/m was the shallowest near 09°N. The low salinity lower than 34.50% was presented in the surface mixed layer between 16°N and 02°N. The conspicuous transitions were formed on each side of the north and south of the low salinity water. The North Equatorial Current was recognized on the north side of 08°N ; the South Equatorial Current near the Equator ; and the North Equatorial Countercurrent in the region between 08°N and 01°N. Several step-like features and inversion layers were presented in the thermocline at the Equator. The lateral advection of water masses in the surface layer was well developed near the Equator. |
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| 内容記述言語 | en | |||||
| 収録雑誌名 |
ja : 鹿児島大学水産学部紀要 en : Memoirs of Faculty of Fisheries Kagoshima University 巻 37, p. 97-109, 発行日 1988-12-25 |
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| 作成日 | ||||||
| 日付 | 1988-12-25 | |||||
| 日付タイプ | Issued | |||||
| ISSN | ||||||
| 収録物識別子タイプ | PISSN | |||||
| ISSN | 0453087X | |||||
| NII書誌ID（雑誌） | ||||||
| 収録物識別子タイプ | NCID | |||||
| NC ID | AN00040498 | |||||
| 出版タイプ | ||||||
| 出版タイプ | VoR | |||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
| NDC | ||||||
| 主題Scheme | NDC | |||||
| 主題 | 660 | |||||
| 公開者・出版者 | ||||||
| 出版者 | 鹿児島大学 | |||||
| 出版者言語 | ja | |||||
| 公開者・出版者 | ||||||
| 出版者 | Kagoshima University | |||||
| 出版者言語 | en | |||||
