Aerological observations over a tropical inland station collected during different phases of the Indian summer monsoon have been used to study the convective mixing in the monsoon boundary layer. The mixing line (ML) model for the thermodynamic structure of a partially cloudy boundary layer has been
On the temperature spectrum in the convective boundary layer
β Scribed by Zbigniew Sorbjan
- Publisher
- Springer
- Year
- 1989
- Tongue
- English
- Weight
- 416 KB
- Volume
- 47
- Category
- Article
- ISSN
- 0006-8314
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β¦ Synopsis
A model for the temperature spectrum in the convective boundary layer is presented. The model is developed by using local similarity parameterization of the mixed layer. The model is compared with an idealized temperature spectrum obtained during the Minnesota experiment and exhibits behavior very similar to that observed in the atmosphere.
π SIMILAR VOLUMES
From sodar measurements gathered during the Voves experiment (France, summer 1977), the variations of the temperature structure parameter C$were studied in the morning planetary boundary layer. Dimensionless profiles of C$ are consistent with the mixed-layer scaling of Kaimal et al. (1976); however,
## Abstract The variation of heat flux with height in inversionβcapped convective boundary layers is discussed. Cospectral shapes at levels above approximately oneβtenth the height of the lowest inversion base (__z__~1~) are shown to depart significantly from surface layer forms. the characteristic
Lumley's model is extended to predict the effect of convection velocity fluctuations on eddy convection velocity for the high-frequency region of the longitudinal, transverse and scalar phase spectra in the atmospheric boundary layer. The resulting model predicts that the eddy convection velocity wi