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    Large-Scale Eddies in the Unstably Stratified Atmospheric Surface Layer. Part I: Velocity and Temperature Structure 

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 024:;page 3537
    Author(s): Wilczak, J. M.
    Publisher: American Meteorological Society
    Abstract: Ensemble vertical cross sections are derived for the velocity and temperature fields associated with large-scale eddy (LSE) temperature ramp structures in the turbulent, convective atmospheric surface layer. The turbulent ...
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    Large-Scale Eddies in the Unstably Stratified Atmospheric Surface Layer. Part II: Turbulent Pressure Fluctuations and the Budgets of Heat Flux, Stress and Turbulent Kinetic Energy 

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 024:;page 3551
    Author(s): Wilczak, J. M.; Businger, Joost A.
    Publisher: American Meteorological Society
    Abstract: A method is developed for retrieving turbulent pressure fluctuations from tower measurements of velocity and temperature, through use of the equations of motion. This method is applied to a series of large-scale eddies ...
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    The Three-Dimensional Structure of Convection in the Atmospheric Surface Layer 

    Source: Journal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 011:;page 2424
    Author(s): Wilczak, J. M.; Tillman, J. E.
    Publisher: American Meteorological Society
    Abstract: During April 1978, a field experiment was undertaken at the Boulder Atmospheric Observatory (BAO), near Boulder, Colorado, to investigate convective plumes in the atmospheric surface layer. The plume translational velocities ...
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    Reply 

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 005:;page 501
    Author(s): Wilczak, J. M.; Businger, J. A.
    Publisher: American Meteorological Society
    Abstract: Abstract not available.
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    Observations and Mixed-Layer Modeling of a Terrain-Induced Mesoscale Gyre: The Denver Cyclone 

    Source: Monthly Weather Review:;1988:;volume( 116 ):;issue: 008:;page 1599
    Author(s): Wilczak, J. M.; Glendening, J. W.
    Publisher: American Meteorological Society
    Abstract: In northeastern Colorado a frequently observed feature of the surface wind field is a stationary, terrain-induced mesoscale gyre, which is often associated with the formation of severe weather. Because of the gyre's proximity ...
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    Observations and Mixed-Layer Modeling of a Terrain-Induced Mesoscale Gyre: The Denver Cyclone 

    Source: Monthly Weather Review:;1988:;volume( 116 ):;issue: 012:;page 2688
    Author(s): Wilczak, J. M.; Glendening, J. W.
    Publisher: American Meteorological Society
    Abstract: In northeastern Colorado a frequently observed feature of the surface wind field is a stationary, terrain-induced mesoscale gyre, which is often associated with the formation of severe weather. Because of the gyre/s proximity ...
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    Thermally Indirect Motions in the Convective Atmospheric Boundary Layer 

    Source: Journal of the Atmospheric Sciences:;1983:;Volume( 040 ):;issue: 002:;page 343
    Author(s): Wilczak, J. M.; Businger, Joost A.
    Publisher: American Meteorological Society
    Abstract: The energetics of the dry convective boundary layer is studied by partitioning the turbulent heat flux into thermally indirect (w???<0) and thermally direct (w???>0) components as a function of z/Zi. It is found that except ...
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    Case Study of an Orographically Induced Mesoscale Vortex (Denver Cyclone) 

    Source: Monthly Weather Review:;1990:;volume( 118 ):;issue: 005:;page 1082
    Author(s): Wilczak, J. M.; Christian, T. W.
    Publisher: American Meteorological Society
    Abstract: Observations taken during the Convection Initiation and Downburst Experiment (CINDE) are used to describe the formation and structure of an orographically induced mesoscale vortex that frequently occurs in northeastern ...
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    Sensitivity of Numerical Simulations to Parameterizations of Roughness for Surface Heat Fluxes at High Winds over the Sea 

    Source: Monthly Weather Review:;2002:;volume( 130 ):;issue: 007:;page 1926
    Author(s): Bao, J-W.; Michelson, S. A.; Wilczak, J. M.
    Publisher: American Meteorological Society
    Abstract: A few roughness length schemes for surface sensible and latent heat fluxes have been developed to fit observations under low and moderate wind (<20 m s?1) conditions. It is not clear to what degree these schemes can be ...
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    Observations and Numerical Model Simulations of the Atmospheric Boundary Layer in the Santa Barbara Coastal Region 

    Source: Journal of Applied Meteorology:;1991:;volume( 030 ):;issue: 005:;page 652
    Author(s): Wilczak, J. M.; Dabberdt, W. F.; Kropfli, R. A.
    Publisher: American Meteorological Society
    Abstract: Observations of boundary-layer flow within the Santa Barbara region taken on 20 September 1985 revel the presence of a wide variety of flow features, including mesoscale wind vortices sea/land breezes, and thermally driven ...
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