A model of a stationary planetary boundary layer is proposed based on the equation of motion with the advective term retained. The latter is modeled by means of the so-called geostrophic momentum approximation in two versions -original and modified. New expressions for the vertical velocity W, at th
A nonlinear treatment of the protocell model by a boundary layer approximation
β Scribed by Kazuaki Tarumi; Helmut Schwegler
- Publisher
- Springer
- Year
- 1987
- Tongue
- English
- Weight
- 564 KB
- Volume
- 49
- Category
- Article
- ISSN
- 1522-9602
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