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    Assessment of Hydrometeor Collection Rates from Exact and Approximate Equations. Part II: Numerical Bounding 

    Source: Journal of Applied Meteorology and Climatology:;2007:;volume( 046 ):;issue: 001:;page 82
    Author(s): Gaudet, Brian J.; Schmidt, Jerome M.
    Publisher: American Meteorological Society
    Abstract: Past microphysical investigations, including Part I of this study, have noted that the collection equation, when applied to the interaction between different hydrometeor species, can predict large mass transfer rates, even ...
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    Low-Level Mesocyclonic Concentration by Nonaxisymmetric Transport. Part I: Supercell and Mesocyclone Evolution 

    Source: Journal of the Atmospheric Sciences:;2006:;Volume( 063 ):;issue: 004:;page 1113
    Author(s): Gaudet, Brian J.; Cotton, William R.
    Publisher: American Meteorological Society
    Abstract: An idealized simulation of a supercell using the Regional Atmospheric Modeling System (RAMS) was able to produce a low-level mesocyclone near the intersection of the forward- and rear-flank downdrafts. The creation of the ...
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    Assessment of Hydrometeor Collection Rates from Exact and Approximate Equations. Part I: A New Approximate Scheme 

    Source: Journal of the Atmospheric Sciences:;2005:;Volume( 062 ):;issue: 001:;page 143
    Author(s): Gaudet, Brian J.; Schmidt, Jerome M.
    Publisher: American Meteorological Society
    Abstract: The collection equation is analyzed for the case of two spherical hydrometeors with collection efficiency unity and exponential size distributions. When the fall velocities are significantly different a more general form ...
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    Low-Level Mesocyclonic Concentration by Nonaxisymmetric Transport. Part II: Vorticity Dynamics 

    Source: Journal of the Atmospheric Sciences:;2006:;Volume( 063 ):;issue: 004:;page 1134
    Author(s): Gaudet, Brian J.; Cotton, William R.; Montgomery, Michael T.
    Publisher: American Meteorological Society
    Abstract: An idealized supercell simulation using the Regional Atmospheric Modeling System (RAMS) produced an elongated low-level mesocyclone that subsequently collapsed into a concentrated vortex. Though vorticity continually ...
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    Submeso Motions within the Stable Boundary Layer and Their Relationships to Local Indicators and Synoptic Regime in Moderately Complex Terrain 

    Source: Journal of Applied Meteorology and Climatology:;2014:;volume( 054 ):;issue: 002:;page 352
    Author(s): Hoover, Joshua D.; Stauffer, David R.; Richardson, Scott J.; Mahrt, Larry; Gaudet, Brian J.; Suarez, Astrid
    Publisher: American Meteorological Society
    Abstract: o better understand the physical processes of the stable boundary layer and to quantify ?submeso motions? in moderately complex terrain, exploratory case-study analyses were performed using observational field data ...
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    Application of the Weather Research and Forecasting Model for Air Quality Modeling in the San Francisco Bay Area 

    Source: Journal of Applied Meteorology and Climatology:;2013:;volume( 052 ):;issue: 009:;page 1953
    Author(s): Rogers, Raphael E.; Deng, Aijun; Stauffer, David R.; Gaudet, Brian J.; Jia, Yiqin; Soong, Su-Tzai; Tanrikulu, Saffet
    Publisher: American Meteorological Society
    Abstract: he Weather Research and Forecasting (WRF) model is evaluated by conducting various sensitivity experiments over central California including the San Francisco Bay Area (SFBA), with the goal of establishing a WRF model ...
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    Numerical Prediction of Submesoscale Flow in the Nocturnal Stable Boundary Layer over Complex Terrain 

    Source: Monthly Weather Review:;2011:;volume( 140 ):;issue: 003:;page 956
    Author(s): Seaman, Nelson L.; Gaudet, Brian J.; Stauffer, David R.; Mahrt, Larry; Richardson, Scott J.; Zielonka, Jeffrey R.; Wyngaard, John C.
    Publisher: American Meteorological Society
    Abstract: umerical weather prediction models often perform poorly for weakly forced, highly variable winds in nocturnal stable boundary layers (SBLs). When used as input to air-quality and dispersion models, these wind errors can ...
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