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Three-dimensional numerical study of turbulence in an entraining mixed layer

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Abstract

The mean structure calculated by a three-dimensional numerical model of a heated planetary boundary layer, in simulation of DAY 33 of the Australian Wangara data, has been previously described. The present study supplements it by describing properties of the calculated turbulence.

A major finding is the importance of entrainment upon turbulence statistics relating to specific humidity, relative to those for potential temperature. The variances, skewness and spectra of velocity, temperature and humidity are presented, as are budget equations for kinetic energy, temperature and humidity variances and heat/moisture fluxes. These are interpreted with regard to the relative importance of the surface flux vs the flux due to entrainment at the top of the mixed layer, and in regard to the structure which would occur if the entrainment were to vanish.

The Rotte-type closure assumption is tested for the correlation between the pressure fluctuation and the vertical gradient of vertical velocity, potential temperature, or specific humidity, and found to be qualitatively correct except near the top of the mixed layer.

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Authors and Affiliations

  1. National Center for Atmospheric Research, Boulder, Colo., USA

    J. W. Deardorff

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  1. J. W. Deardorff
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NCAR is sponsored by the National Science Foundation (U.S.A.).

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Deardorff, J.W. Three-dimensional numerical study of turbulence in an entraining mixed layer. Boundary-Layer Meteorol 7, 199–226 (1974). https://doi.org/10.1007/BF00227913

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  • DOI: https://doi.org/10.1007/BF00227913

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