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The Scaling and Structure of the Estuarine Bottom Boundary Layer
Publisher: American Meteorological Society
Abstract: A two-week dataset from a partially and periodically stratified estuary quantifies variability in the turbulence across the tidal and spring?neap time scales. These observations have been fit with a two-parameter model of ...
Sources of Drag in Estuarine Meanders: Momentum Redistribution, Bottom Stress Enhancement, and Bend-Scale Form Drag
Publisher: American Meteorological Society
Subtidal Salinity and Velocity in the Hudson River Estuary: Observations and Modeling
Publisher: American Meteorological Society
Abstract: A tidally and cross-sectionally averaged model based on the temporal evolution of the quasi-steady Hansen and Rattray equations is applied to simulate the salinity distribution and vertical exchange flow along the Hudson ...
The Temporal Response of the Length of a Partially Stratified Estuary to Changes in River Flow and Tidal Amplitude
Publisher: American Meteorological Society
Abstract: The temporal response of the length of a partially mixed estuary to changes in freshwater discharge Qf and tidal amplitude UT is studied using a 108-day time series collected along the length of the Hudson River estuary ...
Tidal Intrusion Fronts, Surface Convergence, and Mixing in an Estuary with Complex Topography
Publisher: American Meteorological Society
Estuarine Exchange Flow Quantified with Isohaline Coordinates: Contrasting Long and Short Estuaries
Publisher: American Meteorological Society
Abstract: sohaline coordinate analysis is used to compare the exchange flow in two contrasting estuaries, the long (with respect to tidal excursion) Hudson River and the short Merrimack River, using validated numerical models. The ...
Reversed Lateral Circulation in a Sharp Estuarine Bend with Weak Stratification
Publisher: American Meteorological Society
Abstract: AbstractAlthough the hydrodynamics of river meanders are well studied, the influence of curvature on flow in estuaries, with alternating tidal flow and varying water levels and salinity gradients, is less well understood. ...
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