書誌事項
- タイトル別名
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- Abyssal circulation in the Japan Sea.
- 公開日
- 1983
- DOI
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- 10.1007/bf02070392
- 公開者
- 日本海洋学会
この論文をさがす
説明
The water below a depth of 1, 000m in the Japan Sea was found to consist of two water masses, the upper layer (the Deep Water) and the lower layer (the Bottom Water). The boundary of these water masses is marked by discontinuity of potential temperature, dissolved oxygen and silicate at about 2, 000m depth. The mean residence time of the Bottom Water was calculated to be 300 years from analysis of carbon-14 data using a box model. By applying a one dimensional diffusion advection model to the profiles of potential temperature and dissolved oxygen, it was suggested that the upward advection in the Deep Water occurs most intensively in the basin south of the Yamato Rise. The Bottom Water seems to be formed not in the northernmost region of the Japan Sea but in the northwestern area, judging from the distributions of potential temperature and dissolved oxygen.
収録刊行物
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- 日本海洋学会誌
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日本海洋学会誌 39 (5), 220-230, 1983
日本海洋学会
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詳細情報 詳細情報について
-
- CRID
- 1390282681541000320
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- NII論文ID
- 30018375474
- 130003849265
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- ISSN
- 21863113
- 1573868X
- 00298131
- http://id.crossref.org/issn/00298131
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- 本文言語コード
- en
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- データソース種別
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- JaLC
- Crossref
- CiNii Articles
- OpenAIRE
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- 抄録ライセンスフラグ
- 使用不可