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
✦ LIBER ✦
A TKE-dissipation model for the atmospheric boundary layer
✍ Scribed by Anders Andrén
- Publisher
- Springer
- Year
- 1991
- Tongue
- English
- Weight
- 750 KB
- Volume
- 56
- Category
- Article
- ISSN
- 0006-8314
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