York River Destratification: An Estuary-Subestuary Interaction

Science  25 Jun 1982:
Vol. 216, Issue 4553, pp. 1413-1414
DOI: 10.1126/science.216.4553.1413


Destratification in the York River during high spring tides is the result of the interruption of normal two-layer estuarine flow by the advection of relatively fresh water into the river mouth from the Chesapeake Bay. This advection is due to the presence of a longitudinal salinity gradient in the bay and a difference in the tidal current phase between the river and the bay. Similar behavior is seen in other subestuaries of the Chesapeake Bay and may be common in subestuary-estuary interactions.