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オホーツク海への淡水供給量と宗谷暖流の輸送流量について
https://fra.repo.nii.ac.jp/records/2001704
https://fra.repo.nii.ac.jp/records/2001704ed0598fb-b515-490b-970f-8cd55f2ea76b
| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||||||||||||
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| 公開日 | 2024-04-08 | |||||||||||||||||
| タイトル | ||||||||||||||||||
| タイトル | オホーツク海への淡水供給量と宗谷暖流の輸送流量について | |||||||||||||||||
| 言語 | ja | |||||||||||||||||
| タイトル | ||||||||||||||||||
| タイトル | Fresh water supply to the Sea of Okhotsk and volume transport of Soya Warm Current | |||||||||||||||||
| 言語 | en | |||||||||||||||||
| 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 | |||||||||||||||||
| アクセス権 | ||||||||||||||||||
| アクセス権 | metadata only access | |||||||||||||||||
| アクセス権URI | http://purl.org/coar/access_right/c_14cb | |||||||||||||||||
| 著者 |
青田, 昌秋
× 青田, 昌秋
× 石川, 正雄
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| 抄録 | ||||||||||||||||||
| 内容記述タイプ | Abstract | |||||||||||||||||
| 内容記述 | The Sea of Okhotsk is the southernmost freezing sea in the northern hemisphere. The main cause of the sea ice generation in the Sea of Okhotsk is the presence of the low salinity surface layer about 30-60m thick. As the results of ice growth, the convection in winter and the melting of ice in spring, the typical water structure in the Sea of Okhotsk is formed. By the water exchange with the Sea of Okhotsk and the Pacific Ocean through the Kuril Straits, the Oyashio Water is developed. However, there are a number of unclarified points regarding the volume of fresh water supply to the Sea of Okhotsk and the volume of water exchange between the Sea of Okhotsk and the Pacific Ocean. As a preliminary study of the mass and salt budget of the Sea of Okhotsk, the volume of fresh water supply to the Sea of Okhotsk and the volume transport of Soya Warm Current (a branch of the Tsushima Current) were estimated. The fresh water supply was calculated based on the annual precipitation data (Alissow, B. P., et al. 1962) (Fig.2), annual evaportranspiration data (Zubenok, I. et al. 1977) (Fig3) and the report of the discharges of selected rivers of the world (Unesco Press 1974). The volume transport of the Soya Warm Current is estimated from the water level difference between the Japan Sea and the Sea of Okhotsk (Aota, M. et al. 1990) (Fig.1). The results are shown below, Annual fresh water supply : 845km3/year Annual volume transport of Soya Warm Current : 20000Km3/year 37 per cent of the fresh water supply to the Sea of Okhotsk is supplied from the river Amur. | |||||||||||||||||
| 言語 | en | |||||||||||||||||
| 書誌情報 |
ja : 北海道区水産研究所研究報告 en : Bulletin of the Hokkaido National Fisheries Research Institute 巻 55, p. 109-113, ページ数 5, 発行日 1991-03 |
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| 出版者 | ||||||||||||||||||
| 出版者 | 北海道区水産研究所 | |||||||||||||||||
| 言語 | ja | |||||||||||||||||
| 出版者 | ||||||||||||||||||
| 出版者 | Hokkaido National Fisheries Research Institute | |||||||||||||||||
| 言語 | en | |||||||||||||||||
| ISSN | ||||||||||||||||||
| 収録物識別子タイプ | PISSN | |||||||||||||||||
| 収録物識別子 | 0513-2541 | |||||||||||||||||
| 書誌レコードID | ||||||||||||||||||
| 収録物識別子タイプ | NCID | |||||||||||||||||
| 収録物識別子 | AN1015410X | |||||||||||||||||
| 情報源 | ||||||||||||||||||
| 識別子タイプ | Local | |||||||||||||||||
| 関連識別子 | hnf_k_55_8 | |||||||||||||||||
| 関連サイト | ||||||||||||||||||
| 識別子タイプ | URI | |||||||||||||||||
| 関連識別子 | https://agriknowledge.affrc.go.jp/RN/2010501380 | |||||||||||||||||
| 言語 | ja | |||||||||||||||||
| 関連名称 | 日本農学文献記事索引(agriknowledge) | |||||||||||||||||
