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A simple, steady-state, numerical model is used to examine the Rossby-number similarity theory of the atmospheric boundary layer over a slightly inclined terrain. The model confirms the similarity predictions. The slope-influenced universal profiles of the wind velocity defects and the stress components are obtained by the model simulation.
A simple, steady-state, numerical model is used to examine the Rossby-number similarity theory of the atmospheric boundary layer over a slightly inclined terrain. The model confirms the similarity predictions. The slope-influenced universal profiles of the wind velocity defects and the stress components are obtained by the model simulation.
| All Time | Past Year | Past 30 Days | |
|---|---|---|---|
| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 538 | 405 | 146 |
| PDF Downloads | 29 | 11 | 1 |
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