A mean-gradient model of the dry convective boundary layer

Wang Shouping Wang, Bruce A Albrecht

Research output: Contribution to journalArticle

17 Citations (Scopus)

Abstract

A mean-gradient model of the dry convective boundary layer is developed using a convective mass flux representation of the turbulent fluxes. A top-hat model of thermals is used to represent the average characteristics of updrafts and downdrafts in the buoyantly driven circulation. The convective mass flux is related to the convective velocity scale. Although the model is computationally simple, it describes the basic structure of the CBL. In this parameterization the vertical gradients of conserved variables are controlled by internal mixing through vertical mass transports inside the convective boundary layer, bottom mixing due to the surface processes, top mixing due to the entrainment, and lateral mixing between updrafts and downdrafts. -Authors

Original languageEnglish (US)
Pages (from-to)126-138
Number of pages13
JournalJournal of the Atmospheric Sciences
Volume47
Issue number1
StatePublished - 1990
Externally publishedYes

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convective boundary layer
updraft
mass transport
entrainment
parameterization

ASJC Scopus subject areas

  • Atmospheric Science

Cite this

Shouping Wang, W., & Albrecht, B. A. (1990). A mean-gradient model of the dry convective boundary layer. Journal of the Atmospheric Sciences, 47(1), 126-138.

A mean-gradient model of the dry convective boundary layer. / Shouping Wang, Wang; Albrecht, Bruce A.

In: Journal of the Atmospheric Sciences, Vol. 47, No. 1, 1990, p. 126-138.

Research output: Contribution to journalArticle

Shouping Wang, W & Albrecht, BA 1990, 'A mean-gradient model of the dry convective boundary layer', Journal of the Atmospheric Sciences, vol. 47, no. 1, pp. 126-138.
Shouping Wang, Wang ; Albrecht, Bruce A. / A mean-gradient model of the dry convective boundary layer. In: Journal of the Atmospheric Sciences. 1990 ; Vol. 47, No. 1. pp. 126-138.
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