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    Turbulence within a Baroclinic Laboratory Mixed Layer above a Sloping Surface 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 004:;page 772
    Author(s): Deardorff, J. W.; Willis, G. E.
    Publisher: American Meteorological Society
    Abstract: A convection tank (of water) containing a buoyancy-driven turbulent boundary layer was tilted at a 10° angle so that mean-flow shear would occur. This caused shear-stress turbulence production to exceed buoyant production ...
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    A Laboratory Model of the Unstable Planetary Boundary Layer 

    Source: Journal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 005:;page 1297
    Author(s): Willis, G. E.; Deardorff, J. W.
    Publisher: American Meteorological Society
    Abstract: Experimental details of a laboratory model of the unstable planetary boundary layer are given. Measurements of vertical profiles of mean temperature and heat flux, and of velocity and temperature fluctuations are presented ...
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    A Parameterization of Diffusion into the Mixed Layer 

    Source: Journal of Applied Meteorology:;1975:;volume( 014 ):;issue: 008:;page 1451
    Author(s): Deardorff, J. W.; Willis, G. E.
    Publisher: American Meteorological Society
    Abstract: The diffusion from a source near the ground into the daytime mixed layer has been deduced from laboratory measurements, making use of boundary-layer free-convection similarity scaling. A parameterization is presented which ...
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