Numerical Analysis of Formation Mechanism of Intermittent Subsurface-layer Hypoxia in Summer in Ise Bay
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- KAWASAKI Koji
- Nagoya University
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- TODA Keisuke
- Central Japan Railway Company
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- FUJIWARA Tateki
- Kyoto University
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- YOSHIOKA Noriya
- Japan Meteorological Agency
Bibliographic Information
- Other Title
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- 夏季の伊勢湾における間欠的中層貧酸素水塊の形成メカニズムに関する数値的検討
- カキ ノ イセワン ニ オケル カンケツ テキチュウソウヒンサンソスイカイ ノ ケイセイ メカニズム ニ カンスル スウチテキ ケントウ
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Abstract
This study is aimed at numerically discussing the formation mechanism of intermittent subsurface-layer hypoxia in summer season in Ise bay. The long-term variation of hypoxia was examined by using a quasi three-dimensional numerical ocean model with MOVE-WNP data, which are dataset of an ocean variational estimation system in Western North Pacific. The numerical result revealed that hypoxia in the subsurface-layer was formed by the intermittent intrusion of oceanic water into the bottom layer of the bay. The MOVE-WNP data were also confirmed to be useful in comprehending the influence of ocean on internal structure in a bay through the numerical experiments.
Journal
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- Journal of Japan Society of Civil Engineers, Ser. B2 (Coastal Engineering)
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Journal of Japan Society of Civil Engineers, Ser. B2 (Coastal Engineering) 66 (1), 1056-1060, 2010
Japan Society of Civil Engineers
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Keywords
Details 詳細情報について
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- CRID
- 1390282680297143936
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- NII Article ID
- 130004956446
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- NII Book ID
- AA12508551
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- ISSN
- 18838944
- 18842399
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- NDL BIB ID
- 11236630
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- Text Lang
- en
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- Data Source
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- JaLC
- NDL
- Crossref
- CiNii Articles
- KAKEN
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- Abstract License Flag
- Disallowed