Boundary-Layer Meteorology

, Volume 7, Issue 1, pp 81–106

Three-dimensional numerical study of the height and mean structure of a heated planetary boundary layer

  • J. W. Deardorff
Article

DOI: 10.1007/BF00224974

Cite this article as:
Deardorff, J.W. Boundary-Layer Meteorol (1974) 7: 81. doi:10.1007/BF00224974

Abstract

The heated boundary layer for DAY 33 of the Wangara data of southeast Australia (Clarke et al., 1971) is studied numerically with a three-dimensional model using 64000 grid points within a volume 5 km on a side and 2 km deep. Subgrid-scale transport equations were utilized in place of eddy-coefficient formulations. The rate of growth of the mixed layer is examined and parameterized, and the vertical profiles of heat flux, moisture flux and momentum fluxes are examined. The momentum boundary layer is found to coincide essentially with the mixed layer, and to grow with the latter during the hours of solar heating of the surface.

Copyright information

© D. Reidel Publishing Company 1974

Authors and Affiliations

  • J. W. Deardorff
    • 1
  1. 1.National Center for Atmospheric ResearchBoulderUSA