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  1. 139 大気海洋研究所
  2. 80 国際沿岸海洋研究センター
  3. Coastal Marine Science
  4. 34
  5. 1
  1. 0 資料タイプ別
  2. 30 紀要・部局刊行物
  3. Coastal Marine Science
  4. 34
  5. 1

Impact of sporadically enhanced river discharge on the climatological distribution of river water in Suruga Bay

https://doi.org/10.15083/00040664
https://doi.org/10.15083/00040664
8c97c5a0-b686-43ce-b22b-52bbd6007c66
名前 / ファイル ライセンス アクション
CMS340101.pdf CMS340101.pdf (1.7 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2012-05-25
タイトル
タイトル Impact of sporadically enhanced river discharge on the climatological distribution of river water in Suruga Bay
言語
言語 eng
キーワード
主題Scheme Other
主題 river water spreading
キーワード
主題Scheme Other
主題 sporadically enhanced discharge
キーワード
主題Scheme Other
主題 Suruga Bay
キーワード
主題Scheme Other
主題 numerical experiment
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
ID登録
ID登録 10.15083/00040664
ID登録タイプ JaLC
著者 Tanaka, Kiyoshi

× Tanaka, Kiyoshi

WEKO 93496

Tanaka, Kiyoshi

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Michida, Yutaka

× Michida, Yutaka

WEKO 93497

Michida, Yutaka

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Komatsu, Teruhisa

× Komatsu, Teruhisa

WEKO 93498

Komatsu, Teruhisa

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著者所属
著者所属 Center for Advanced Marine Research, Ocean Research Institute, The University of Tokyo
著者所属
著者所属 International Coastal Research Center, Ocean Research Institute, The University of Tokyo
著者所属
著者所属 Department of Marine Bioscience, Ocean Research Institute, The University of Tokyo
抄録
内容記述タイプ Abstract
内容記述 In Suruga Bay the river discharge is sporadically enhanced by heavy rainfall, and its daily mean values often exceed by an order of magnitude the seasonal means. We have therefore investigated the impact of the sporadically enhanced river discharge on the climatological distribution of river water in Suruga Bay, performing numerical experiments with an ocean general circulation model. As the river discharge is enhanced, a larger amount of the Coastal Water (defined by salinity less than 33.0) is exported out of shallow areas such as the continental shelf, being less trapped by the bottom topography. Moreover, the high frequency (day-scale) variation in the river discharge causes large temporal variations of the surface salinity distribution in the bay. However, it has only a minor influence in the time-averaged field (under the same condition in terms of the total amount of the discharged river water). It is therefore suggested that in the actual sea, the high frequency (day-scale) variability in the river discharge has only a minor influence on the climatological distribution of river water in the bay.
書誌情報 Coastal marine science

巻 34, 号 1, p. 1-6, 発行日 2010-08-20
ISSN
収録物識別子タイプ ISSN
収録物識別子 13493000
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AA11957899
日本十進分類法
主題Scheme NDC
主題 452
出版者
出版者 International Coastal Research Center, Atmosphere and Ocean Research Institute, the University of Tokyo
出版者別名
東京大学大気海洋研究所国際沿岸海洋研究センター
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