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- W1852418937 abstract "The influence of tides on estuarine processes has long been of interest to estuarine hydrographers and biologists. Recently it was shown that moderately stratified subestuaries of the lower Chesapeake Bay undergo periodic destratification (i.e. surface to bottom salinity differences less than 1 per mille) which correlate with the occurrence of high spring tides (Haas, 1977). In the York River, destratification events were reported to persist for up to three days and result in near vertical homogeneity. Subsequent observations indicated that destratification is preceded by the influx of less saline water into the mouth of the River, an occurrence suggested as instrumental in the subsequent destratification processes (Hayward et al., 1982).KeywordsWind StressTidal RangeTidal HeightSalinity DifferenceGloucester PointThese keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves." @default.
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- W1852418937 date "1986-01-01" @default.
- W1852418937 modified "2023-09-27" @default.
- W1852418937 title "Empirical Models of Stratification Variation in the York River Estuary, Virginia, USA" @default.
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- W1852418937 doi "https://doi.org/10.1007/978-1-4612-4966-5_14" @default.
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