Contribution to the hydrobiology of the York River: predicting surface mixed layer depth (destratification, tidal, semilunar, Virginia)
Destratification in the York River, USA, during high spring tides is the result of the interruption of normal two-layer estuarine flow by advection of relatively fresh water in to the River mouth from the Chesapeake Bay. This is due to the presence of a longitudinal salinity gradient in the Bay and...
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| Format: | Others |
| Language: | English |
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W&M ScholarWorks
1986
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| Online Access: | https://scholarworks.wm.edu/etd/1539616690 https://scholarworks.wm.edu/cgi/viewcontent.cgi?article=2257&context=etd |