WEKO3
アイテム
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内湾の熱収支と貧酸素水塊の形成について
http://hdl.handle.net/10649/136
http://hdl.handle.net/10649/136046dc235-3b58-46f2-a0f8-586a50aed1c1
名前 / ファイル | ライセンス | アクション |
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K11_10.pdf (1.4 MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2011-02-14 | |||||
タイトル | ||||||
タイトル | 内湾の熱収支と貧酸素水塊の形成について | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Anoxia | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | coastal sea | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | heat exchange | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | density stratification | |||||
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 |
中村, 由行
× 中村, 由行× 一宮, 大祐× 早川, 典生× 西村, 肇 |
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著者別名 | ||||||
識別子Scheme | WEKO | |||||
識別子 | 1848 | |||||
姓名 | ナカムラ, ヨシユキ | |||||
著者別名 | ||||||
識別子Scheme | WEKO | |||||
識別子 | 1849 | |||||
姓名 | イチミヤ, ダイスケ | |||||
著者別名 | ||||||
識別子Scheme | WEKO | |||||
識別子 | 1850 | |||||
姓名 | ハヤカワ, ノリオ | |||||
著者別名 | ||||||
識別子Scheme | WEKO | |||||
識別子 | 1851 | |||||
姓名 | ニシムラ, ハジメ | |||||
著者別名 | ||||||
識別子Scheme | WEKO | |||||
識別子 | 1852 | |||||
姓名 | Nakamura, Yoshiyuki | |||||
著者別名 | ||||||
識別子Scheme | WEKO | |||||
識別子 | 1853 | |||||
姓名 | Ichimiya, Daisuke | |||||
著者別名 | ||||||
識別子Scheme | WEKO | |||||
識別子 | 1854 | |||||
姓名 | Hayakawa, Norio | |||||
著者別名 | ||||||
識別子Scheme | WEKO | |||||
識別子 | 1855 | |||||
姓名 | Nishimura, Hajime | |||||
著者所属 | ||||||
値 | 長岡技術科学大学建設系 | |||||
著者所属 | ||||||
値 | 兵庫県 | |||||
著者所属 | ||||||
値 | 長岡技術科学大学建設系 | |||||
著者所属 | ||||||
値 | 東京大学工学部化学工学科 | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Field data on coastal anoxia observed during nine years in Osaka Bay were analyzed and examined using a numerical method. Field data suggest that the development of thermal stratification in the middle layer and the subsequent retardation of oxygen transport to the bottom layer is the principle mechanism in the formation of anoxia in the bottom water. The numerical model, which was developed by Nakamura and Nishimura to predict the changes of temperature and oxygen distribution, has been improved by taking account of heat exchange through the air-water interface. The improved model well reproduces the characteristic temperature variation and the dissolved oxygen content in the bottom field condition during the stratification period as well as the mixing period in autumn. Important parameters for the determination of surface heat exchange have further been evaluated by sensitivity analyses. The results show that the vapor pressure in the atmosphere and the wind velocity are the most sensitive to the total heat flux. | |||||
書誌情報 |
長岡技術科学大学研究報告 巻 11, p. 69-81, 発行日 1989-10 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0388-5631 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00177120 | |||||
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 | |||||
その他のタイトル | ||||||
その他のタイトル | Sea surface heat transfer and its effects on the formation of coastal bay anoxia | |||||
出版者 | ||||||
出版者 | 長岡技術科学大学 |