Estuarine Stratification
Estuarine Stratification is a hydrodynamic phenomenon characterized by the vertical layering of water masses in an estuary due to gradients in salinity and temperature, which results in limited mixing between the fresher, lighter surface water and the denser, more saline bottom water.
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Freshwater Discharge EffectsHalocline DynamicsHorizontal Stratification VariabilityLongitudinal Stratification GradientsPycnocline StructureSeasonal Stratification VariabilityStratification BreakdownStratification Under Drought ConditionsStratification Under River FloodsThermocline Structure
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NEW DIMENSIONS IN ESTUARY CLASSIFICATION1
Donald V. Hansen, Maurice Rattray · Limnology and Oceanography · 1966 · 683 citations · Full text
W. Rockwell Geyer, Parker MacCready · Annual Review of Fluid Mechanics · 2013 · 629 citations · Full text
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Woods Hole Oceanographic Institution, United States
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Woods Hole Oceanographic Institution
Falmouth, United States
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59 publications
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East China Normal University
Shanghai, China
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32 publications
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William & Mary
Williamsburg, United States
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United States Geological Survey
Reston, United States
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University of Washington
Seattle, United States
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Ruđer Bošković Institute
Zagreb, Croatia
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University of Maryland Center for Environmental Science
Cambridge, United States
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Centre National de la Recherche Scientifique
Paris, France
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JGR · 39 publications · 3.4K citations
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