Computation of wind flow over topography
β Scribed by D.A Paterson; J.D Holmes
- Publisher
- Elsevier Science
- Year
- 1993
- Tongue
- English
- Weight
- 243 KB
- Volume
- 46-47
- Category
- Article
- ISSN
- 0167-6105
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π SIMILAR VOLUMES
The reduced model for a large ice sheet Β―ow is uniformly valid when the bed topography is Β―at or has slopes relative to the horizontal no greater than order e, where e 2 is a very small dimensionless viscosity based on the geometry and Β―ow parameters. Real beds will have much greater slopes, of orde
over an obstacle is the production of lee waves, which can persist for long distances downstream, making the use of A robust multigrid method for the incompressible Navier-Stokes equations is presented and applied to the computation of viscous stretched grids unavoidable. When lee wave amplitudes fl