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    Transport and Diffusion in the Transition Layer and Planetary Boundary Layer for Drainage Flows in Anderson and Putah Creeks, California, during ASCOT 1980 

    Source: Journal of Climate and Applied Meteorology:;1984:;volume( 023 ):;issue: 005:;page 812
    Author(s): Fosberg, Michael A.
    Publisher: American Meteorological Society
    Abstract: Approximately 100 constant-volume, superpressured balloons (tetroons) were tracked in the Anderson and Putah Creek drainages of the Geysers geothermal area of northern California as part of the ASCOT (Atmospheric Studies ...
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    Numerical Analysis of Convective Motions over a Mountain Ridge 

    Source: Journal of Applied Meteorology:;1967:;volume( 006 ):;issue: 005:;page 889
    Author(s): Fosberg, Michael A.
    Publisher: American Meteorological Society
    Abstract: The convection associated with a valley wind regime was analyzed by numerical techniques. The Boussinesq equations and their energy properties were used to define the terms computed from observed data. The numerical results ...
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    Airflow Over a Heated Coastal Mountain 

    Source: Journal of Applied Meteorology:;1969:;volume( 008 ):;issue: 003:;page 436
    Author(s): Fosberg, Michael A.
    Publisher: American Meteorological Society
    Abstract: Observations of airflow over the Santa Ana Mountains were analyzed by numerical techniques. The Boussinesq equations and their energy properties were used to define the terms computed from the observed data. The numerical ...
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    Marine Air Penetration in Central California 

    Source: Journal of Applied Meteorology:;1966:;volume( 005 ):;issue: 005:;page 573
    Author(s): Fosberg, Michael A.; Schroeder, Mark J.
    Publisher: American Meteorological Society
    Abstract: Three-dimensional analysis shows the sea-breeze front to be primarily a wind shift line in which the thermal discontinuity lags behind the shear line and becomes quasi-stationary in the afternoon. Two synoptic patterns ...
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