Titlebook: Residual Currents and Long-term Transport; R. T. Cheng Book 1990 Springer-Verlag New York, Inc. 1990 Coast.ecosystem.evolution.marine.mode

LVAD360

Paleontology

改變立場

Longitudinal Dispersion of Salt in the Volkerak Estuarydal regime and freshwater discharge for the estuary are controlled by respectively a storm surge barrier and discharge sluices. In the different experiments freshwater discharges are 25 m./s, 50 m./s and 100 m./s and the tidal ranges at the mouth are 2.70 m and 3.50 m. In the seaward part of the est

Contort

Mixing and Trapping in Australian Tropical Coastal Watershe coastal boundary layer inhibits mixing between the nearshore and offshore water by two effects, firstly by trapping in mangrove swamps, and secondly due to frictional effects which inhibit inertial jets. Contrast was found between coastal boundary layer dynamics in the Gulf of Carpentaria, which

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Control of Estuarine Salinities by Coastal Ocean Salinityuarine salinities against Mississippi River discharge and cross-spectrum analysis do not produce a successful hindcast of the observations. Parsimonious auto-regressive, moving-average predictive models of the weekly-averaged salinity data are quite skillful in hindcasting the measurements. These mo

祖先

Mixing Processes in a Numerical Model of the Western Dutch Wadden Seaian displacement of watermasses appears to be very sensitive to the time of release, the initial position and the initial volume of the watermass considered. The advective component of this displacement agrees with the Eulerian residual currents on relatively large scales. In a Lagrangian sense the

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BOAST

Dorsal

支架

Residual Currents and Long-term Transport978-1-4613-9061-9Series ISSN 0724-5890