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The plume of Mississippi and Atchafalaya River system (MARS) is normally confined to the continental shelf and extends westward. During March 2010, while weather in North America was dominated by unu...
The present study demonstrates that the spectral slope coefficient of chromophoric dissolved organic matter(CDOM) between 275 nm and 295 nm (S275–295) can be used as a tracer of the percent terrigenou...
Dispersion of freshwater mussel larvae in a lowland river     a lowland river  freshwater       font style='font-size:12px;'> 2014/4/16
We examined the dispersal of larvae (glochidia) of a common unionid mussel species, Actinonaias ligamentina, which need to attach to a host fish in order to develop into juveniles, in a lowland river...
Atmospherically driven flow in the Providence River (a partially mixed estuary) has been examined using a 51-day velocity record measured 2 m from the bottom. Velocity fluctuations at time scales betw...
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...
The pressure field over a sloping continental shelf subject to freshwater runoff at the coast can be resolved into a nearly two-dimensional dynamic height field and a residual field, the latter arisin...
The Influence of Wind Stress and River Runoff on a Shelf-Sea Front     Wind Stress  River Runoff  Shelf-Sea Front       font style='font-size:12px;'> 2009/1/20
Runoff from land gives rise to the formation of a front-jet system separating fresher coastal waters from more saline waters offshore, over some continental shelves, notably in the Mid-Atlantic Bight ...
A unique set of field observations has documented intense wave–current–bathymetry interactions in a tidal inlet, providing a severe test of existing wave theory. Hourly wave spectral estimates were ac...
River-Forced Estuarine Plumes     river-forced estuarine plumes  seaward sloping bottom       font style='font-size:12px;'> 2009/1/5
The development, maintenance, and dissipation of river-forced estuarine plumes with and without seaward sloping bottom are studied by use of a three-dimensional, primitive-equation model. Inside the e...
The Formation and Fate of a River Plume:A Numerical Model     free frontal boundary  Numerical Model       font style='font-size:12px;'> 2008/12/27
A mathematical model that describes the formation and dilution of a frontally bounded river plume is presented. Such features were first studied at the mouth of the Connecticut River during periods of...
Convergence and Downwelling at a River Plume Front     Convergence  Downwelling  River Plume Front       font style='font-size:12px;'> 2008/10/27
The small-scale structure of the circulation and hydrography at the frontal boundary of the Connecticut River plume in Long Island Sound has been resolved using a novel combination of instrument...
Estuarine Adjustment to Changes in River Flow and Tidal Mixing     Estuarine Adjustment  Changes  River Flow  Tidal Mixing       font style='font-size:12px;'> 2008/7/10
The adjustment of estuarine circulation and density to changes in river flow and tidal mixing is investigated using analytical and numerical models. Tidally averaged momentum and salinity equations in...
The alongshore transport of a surface-trapped river plume is studied using a three-dimensional model. Model simulations exhibit the previously observed rightward veering (in the Northern Hemisphere) o...
We performed multispectral, in situ fluorescence measurements of detrital colored organic matter (COM) and chlorophyll a (Chl a) in surface waters of the West Florida Shelf using the Wet Labs spectral...

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