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Short Contribution

A note on the closure in Lilly-type inversion models

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Pages 284-288 | Received 23 Sep 1977, Published online: 15 Dec 2016

References

  • Ball, F. K. 1960. Control of inversion height by surface heating. Quart. J. R. Met. Soc. 86, 483–494.
  • Cattle, H. and Weston, K. J. 1975. Budget studies of heat flux profiles in the convective boundary layer overland. Quart. J. R. Met. Soc. 101, 353–363.
  • Deardorff, J. W., Willis, G. E. and Lilly, D. K. 1969. Laboratory investigation of non-steady penetrative convection. J. Fluid. Mech. 35, 7–31.
  • Deardorff, J. W. 1976. On the entrainment rate of a stratocumulus-topped mixed layer. Quart. J. R. Met. Soc. 102, 563–582.
  • Kraus, H. and Schaller, E. 1978. Steady-state charac-teristics of inversions capping a well-mixed PBL. Boundary-Layer MeteoroL 14, 83–104.
  • Lilly, D. K. 1968. Models of cloud-topped mixed layers under a strong inversion. Quart. J. R. Met. Soc. 94, 292–309.
  • Schubert, W. H. 1976. Experiments with Lilly's cloud-topped mixed layer model. J. Atmos. ScL 33, 436–446.
  • Stull, R. B. 1976. The energetics of entrainment across a density interface. J. Atmos. Sci. 33, 1260–1267.
  • Zeman, O. and Tennekes, H. 1977. Parameterization of the turbulent energy budget at the top of the daytime atmospheric boundary layer. J. Atmos. Sci. 34, 111–123.