Abstract A high-order model is proposed for the study of the 24 h evolution of clear planetary boundary layers. The model includes the rate equations of correlations up to the third order, as required for an accurate description of daytime convective phenomena, but it also takes into account interactions between radiative transfer and turbulence in order to achieve a physically reasonable description of the nocturnal structure of the boundary layer. This numerical model is tested against the Wangara boundary layer data of Day 33 and Night 33–34 (Clarke et al., 197l). The computed daytime mean structure of the boundary layer compares favorably with the Wangara data, while the daytime turbulent structure, expressed in the framework of the convective similarity theory, is in particularly good quantitative agreement with a number of experimental and numerical data concerning convection in the boundary layer, with particular concern to the production of turbulence at the top of the mixed layer. The computed no...
CITATION STYLE
André, J. C., De Moor, G., Lacarrère, P., & du Vachat, R. (1978). Modeling the 24-Hour Evolution of the Mean and Turbulent Structures of the Planetary Boundary Layer. Journal of the Atmospheric Sciences, 35(10), 1861–1883. https://doi.org/10.1175/1520-0469(1978)035<1861:mtheot>2.0.co;2
Mendeley helps you to discover research relevant for your work.