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Estuarine water circulation is controlled by the inflow of rivers, the tides, rainfall and evaporation, the wind, and other oceanic events such as an upwelling, an eddy, and storms. Estuarine water circulation patterns are influenced by vertical mixing and stratification, and can affect residence time and exposure time.

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  • Estuarine water circulation (en)
  • 塩水くさび (ja)
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  • Estuarine water circulation is controlled by the inflow of rivers, the tides, rainfall and evaporation, the wind, and other oceanic events such as an upwelling, an eddy, and storms. Estuarine water circulation patterns are influenced by vertical mixing and stratification, and can affect residence time and exposure time. (en)
  • 塩水くさび(えんすいくさび)とは、河川や帯水層中に海水が遡上し、基底部付近に塩分濃度の高い層を造る現象である。 (ja)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/EstauryModel.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/FjordCirculation.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/PartiallyMixedEstuary.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/SaltWedgeEstuary.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Vertically_Homogeneous_Estuary.jpg
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  • Estuarine water circulation is controlled by the inflow of rivers, the tides, rainfall and evaporation, the wind, and other oceanic events such as an upwelling, an eddy, and storms. Estuarine water circulation patterns are influenced by vertical mixing and stratification, and can affect residence time and exposure time. (en)
  • 塩水くさび(えんすいくさび)とは、河川や帯水層中に海水が遡上し、基底部付近に塩分濃度の高い層を造る現象である。 (ja)
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