MORWIN: Collaborative Modeling of Coastal Morphodynamics

Observing Changes in an Ebb-Tidal Shoal

Flood Shoal Response to Inlet Modifications at Barnegat Inlet, New Jersey

Bathymetric Change Off the Washington?Oregon Coast

Scales of Variability along the Columbia River Littoral Cell

Development and Study of Green's Function for Water Waves Over Variable Bathymetry Domains

Quantitative Estimations of Bar Dynamics from Video Images

Cyclic Bar Behavior Viewed by Video Imagery

Variations of Breaking Wave Statistics Across the Nearshore Zone

Tide Induced Mass-Flux in Shallow Estuaries

Combined Refraction-Diffraction - Wave-Current Interaction Over a Complex Nearshore Bathymetry

Longshore Currents Over Barred Beaches

Beach Profile Evolution Under Mean Conditions

Numerical Simulation of Internal Kelvin Waves with Z-level and Sigma Level Models

An Evaluation of Tidal Predictions in the Yellow and East China Seas

Detailed Measurements of Scour at Bridges
The U.S. Geological Survey, in cooperation with the Federal Highway Administration, has recently developed equipment and techniques for collecting detailed bathymetric and hydraulic data...

The Use of an Equivalent Porosity Method to Model Flow in Marshes
Two dimensional modeling of marshes under unsteady flow conditions often involves description of sections that alternately wet and dry. The equivalent porosity method (King and Roig, 1988;...

Boundary Forcing and a Dual-Mode Calculation Scheme for Coastal Tidal Models Using Step-Wise Bathymetry
Tidal energetics are persistent and important factors in almost all coastal regions. As such, it is important to employ techniques that can consistently reproduce observed tidal variations....

The Numerical Simulation of Wetting and drying Areas using Riemann Solvers

Recent Applications of Acoustic Doppler Current Profilers
A Broadband acoustic Doppler current profiler (BB-ADCP) is a new instrument being used by the U.S. Geological Survey (USGS) to measure stream discharge and velocities, and bathymetry....

 

 

 

 

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