The Community Sediment Transport Modeling System (CSTMS) cohesive bed sub-model that accounts for erosion, deposition, consolidation, and swelling was implemented in a three-dimensional domain to represent the York River estuary, Virginia. The objectives of this paper are to (1) describe the application of the three-dimensional hydrodynamic York Cohesive Bed Model, (2) compare calculations to observations, and (3) investigate sensitivities of the cohesive bed sub-model to user-defined parameters. Model results for summer 2007 showed good agreement with tidal-phase averaged estimates of sediment concentration, bed stress, and current velocity derived from Acoustic Doppler Velocimeter (ADV) field measurements. An important step in implementin...
Appropriate parameterization of time-dependent erodibility of muddy seabeds is a significant barrier...
Numerical simulation on the formation of an Estuarine Turbidity Maximum (ETM) is a difficult task be...
Thesis advisor: Gail C. KinekeThis study characterizes the bed of the Connecticut River estuary in t...
The Community Sediment Transport Modeling System (CSTMS) cohesive bed sub-model that accounts for er...
© The Author(s), 2014. This article is distributed under the terms of the Creative Commons Attributi...
The Community Sediment Transport Modeling System (CSTMS) cohesive bed sub-model that accounts for er...
The Community Sediment Transport Modeling System (CSTMS) cohesive bed sub-model that accounts for er...
In general, the availability of sediment for transport increases with the magnitude of bed shear str...
The York River estuary is a partially mixed semi-diurnal tidal tributary of the Chesapeake Bay with ...
The Community Sediment Transport Modeling System (CSTMS) is being used to represent conditions in th...
The Community Sediment Transport Modeling System (CSTMS) is being used to represent conditions in th...
The York River estuary is categorized as micro-tidal with a tidal range ~0.8 m; however, periodicall...
The York River estuary is categorized as micro-tidal with a tidal range ~0.8 m; however, periodicall...
Particle settling velocity and erodibility are key factors that govern the transport of sediment thr...
Appropriate parameterization of time-dependent erodibility of muddy seabeds is a significant barrier...
Appropriate parameterization of time-dependent erodibility of muddy seabeds is a significant barrier...
Numerical simulation on the formation of an Estuarine Turbidity Maximum (ETM) is a difficult task be...
Thesis advisor: Gail C. KinekeThis study characterizes the bed of the Connecticut River estuary in t...
The Community Sediment Transport Modeling System (CSTMS) cohesive bed sub-model that accounts for er...
© The Author(s), 2014. This article is distributed under the terms of the Creative Commons Attributi...
The Community Sediment Transport Modeling System (CSTMS) cohesive bed sub-model that accounts for er...
The Community Sediment Transport Modeling System (CSTMS) cohesive bed sub-model that accounts for er...
In general, the availability of sediment for transport increases with the magnitude of bed shear str...
The York River estuary is a partially mixed semi-diurnal tidal tributary of the Chesapeake Bay with ...
The Community Sediment Transport Modeling System (CSTMS) is being used to represent conditions in th...
The Community Sediment Transport Modeling System (CSTMS) is being used to represent conditions in th...
The York River estuary is categorized as micro-tidal with a tidal range ~0.8 m; however, periodicall...
The York River estuary is categorized as micro-tidal with a tidal range ~0.8 m; however, periodicall...
Particle settling velocity and erodibility are key factors that govern the transport of sediment thr...
Appropriate parameterization of time-dependent erodibility of muddy seabeds is a significant barrier...
Appropriate parameterization of time-dependent erodibility of muddy seabeds is a significant barrier...
Numerical simulation on the formation of an Estuarine Turbidity Maximum (ETM) is a difficult task be...
Thesis advisor: Gail C. KinekeThis study characterizes the bed of the Connecticut River estuary in t...