Drilldown: BibEntryCargo

From CSDMS
BibEntryCargo > Year: 2011 & Journal : Ocean Dynamics or Water Resources Research

Use the filters below to narrow your results.

Title:
A numerical study of horizontal dispersion in a macro tidal basin (1) · Bed composition generation for morphodynamic modeling: case study of San Pablo Bay in California, USA (1) · Efficient scheme for the shallow water equations on unstructured grids with application to the Continental Shelf (1) · Far-field effects of tidal energy extraction in the Minas Passage on tidal circulation in the Bay of Fundy and Gulf of Maine using a nested-grid coastal circulation model (1) · Flow over a rounded backward-facing step, using a z-coordinate model and a σ-coordinate model (1) · Fully coupled approach to modeling shallow water flow, sediment transport, and bed evolution in rivers: SHALLOW WATER FLOW AND SEDIMENT TRANSPORT IN RIVERS (1) · Hyporheic flow path response to hydraulic jumps at river steps: Hydrostatic model simulations: HYPORHEIC RESPONSE TO HYDRAULIC JUMPS (1) · Impact of climate change on the hydroclimatology of Lake Tana Basin, Ethiopia: IMPACT OF CHANGING CLIMATE ON WATER RESOURCES (1) · Numerical modelling of organic waste dispersion from fjord located fish farms (1) · Numerical simulation of internal solitary wave—induced reverse flow and associated vortices in a shallow, two-layer fluid benthic boundary layer (1) · Simulation and detection of tsunami signatures in ocean surface currents measured by HF radar (1) · Temporal dynamics of model parameter sensitivity for computationally expensive models with the Fourier amplitude sensitivity test: TEMPORAL DYNAMICS OF MODEL PARAMETER SENSITIVITY (1) · The significance of turbulent flow representation in single-continuum models: TURBULENT FLOW IN SINGLE-CONTINUUM MODELS (1)
Editors:
Journal: (Click arrow to add another value)
Booktitle:
Volume:
ISBN:

Showing below up to 13 results in range #1 to #13.

View (previous 250 | next 250) (20 | 50 | 100 | 250 | 500)


View (previous 250 | next 250) (20 | 50 | 100 | 250 | 500)