A two-part study focusing on the development and application of open boundary conditions (OBCs) for a limited-area high-resolution coastal ocean model off Oregon is pursued. In Part 1, the OBCs are formulated and evaluated in numerical experiments utilizing idealized wind forcing. In Part 2, the OBCs are applied in an experiment with forcing by space and time variable winds obtained from a regional mesoscale atmospheric model. The initial experiments in Part 1 involve forcing by winds that are constant in time and are spatially uniform. The response to both upwelling favorable (southward) and downwelling favorable (northward) winds are examined and compared to results obtained with cyclic alongshore boundary conditions (CBCs). Additional ex...
Atmosphere model-derived flux fields are used to force coastal ocean models. Coarse resolution and i...
Graduation date: 2006The effects of alongshore variability in topography (banks and capes) and spati...
The feasibility of sequential open-boundary control by data assimilation in a regional ocean model h...
copyrighted by American Geophysical UnionTl1is article discusses the results of an experimental surv...
copyrighted by American Geophysical UnionThe objective of this study is to evaluate the performance ...
Time-dependent downwelling on the Oregon continental shelf is studied with a two-dimensional approxi...
copyrighted by American Geophysical UnionThis is the second part of a modeling study of wind-forced ...
[1] Time-dependent, three-dimensional, upwelling circulation on the continental shelf off the Oregon...
[1] Time-dependent, three-dimensional, upwelling circulation on the continental shelf off the Oregon...
copyrighted by American Geophysical UnionA two-part modeling study of the wind-forced flow on the co...
Two-dimensional numerical models were used to further study appropiiate conditions at the open bound...
Open boundaries (OBs) are usually unavoidable in numerical coastal circulation simulations. At OBs, ...
It is impractical to create gridded numerical models of coastal circulation with sufficient resoluti...
Sixty-day simulations of flow on the Oregon continental shelf are performed using the Blumberg and M...
A two-layer model with an idealized continental shelf and slope bottom topography is utilized to stu...
Atmosphere model-derived flux fields are used to force coastal ocean models. Coarse resolution and i...
Graduation date: 2006The effects of alongshore variability in topography (banks and capes) and spati...
The feasibility of sequential open-boundary control by data assimilation in a regional ocean model h...
copyrighted by American Geophysical UnionTl1is article discusses the results of an experimental surv...
copyrighted by American Geophysical UnionThe objective of this study is to evaluate the performance ...
Time-dependent downwelling on the Oregon continental shelf is studied with a two-dimensional approxi...
copyrighted by American Geophysical UnionThis is the second part of a modeling study of wind-forced ...
[1] Time-dependent, three-dimensional, upwelling circulation on the continental shelf off the Oregon...
[1] Time-dependent, three-dimensional, upwelling circulation on the continental shelf off the Oregon...
copyrighted by American Geophysical UnionA two-part modeling study of the wind-forced flow on the co...
Two-dimensional numerical models were used to further study appropiiate conditions at the open bound...
Open boundaries (OBs) are usually unavoidable in numerical coastal circulation simulations. At OBs, ...
It is impractical to create gridded numerical models of coastal circulation with sufficient resoluti...
Sixty-day simulations of flow on the Oregon continental shelf are performed using the Blumberg and M...
A two-layer model with an idealized continental shelf and slope bottom topography is utilized to stu...
Atmosphere model-derived flux fields are used to force coastal ocean models. Coarse resolution and i...
Graduation date: 2006The effects of alongshore variability in topography (banks and capes) and spati...
The feasibility of sequential open-boundary control by data assimilation in a regional ocean model h...