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Non-Tidal Variability in the Chesapeake Bay and Potomac River：Evidence for Non-Local Forcing
Non-Tidal Variability Chesapeake Bay Potomac River Non-Local Forcing
2009/2/23
Non-tidal variability in the Chesapeake Bay and Potomac River, and its relation to atmospheric forcing, is examined from two-month sea level and bottom current measurements. The dominant sea level flu...
Wind-Driven Circulation in the Chesapeake Bay, Winter, 1975
Wind-Driven Circulation Chesapeake Bay
2009/2/13
Nontidal circulation in Chesapeake Bay was examined from one-month current records at 50 and 200 km from the entrance. The monthly mean flow was basically a two-layered circulation; in addition, there...
Subtidal Sea Level Variations in the Chesapeake Bay and Relations to Atmospheric Forcing
Subtidal Sea Level Atmospheric Forcing Chesapeake Bay
2009/2/13
Subtidal sea level variations in the Chesapeake Bay were examined over a one-year period for evidence of wind-driven barotropic circulation. The major transport occurred at time scales of 3–5 days, wh...
Wind-Induced Destratification in Chesapeake Bay
Wind-Induced Destratification Chesapeake Bay
2009/1/9
Multiyear continuous observations of velocity and salinity in the Chesapeake Bay indicate that wind-induced destratification occurs frequently from early fall through midspring over large areas of the...