The heat input into the planetary boundary layer (PBL) resulting from surface-atmosphere interactions under extremely arid conditions is formulated as a linear differential equation. The forcing for this heat input is the product of the shortwave (solar) absorption at the surface and the surfaceto-P
A simple two-layer model of the planetary boundary layer
β Scribed by D. Yordanov
- Publisher
- Springer
- Year
- 1974
- Tongue
- English
- Weight
- 340 KB
- Volume
- 23
- Category
- Article
- ISSN
- 1436-5065
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π SIMILAR VOLUMES
The integrated momentum and thermodynamic equations through the planetary boundary layer (PBL) are solved numerically to predict the mean changes of wind and potential temperature from which surface fluxes are computed using bulk transfer coefficients of momentum and heat. The second part of the stu
## Abstract A simple slab model for the boundary layer of a hurricane is reβexamined and a small error in the original calculation is corrected. With this correction, the development of supergradient winds is a ubiquitous feature of the solutions. The boundary layer shows two types of behaviour in