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    The Role of Negative Buoyancy in Surface-Based Convection and Its Representation in Cumulus Parameterization Schemes 

    Source: Journal of Applied Meteorology and Climatology:;2013:;volume( 052 ):;issue: 012:;page 2887
    Author(s): Ganeshan, Manisha; Murtugudde, Raghu; Strack, John
    Publisher: American Meteorological Society
    Abstract: everal warm season, late-afternoon precipitation events are simulated over the Chesapeake Bay watershed using the Weather Research and Forecasting (WRF) model at three different resolutions. The onset and peak of surface-based ...
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    Sensitivity of Model-Generated Daytime Surface Heat Fluxes over Snow to Land-Cover Changes 

    Source: Journal of Hydrometeorology:;2003:;Volume( 004 ):;issue: 001:;page 24
    Author(s): Strack, John E.; Pielke, Roger A.; Adegoke, Jimmy
    Publisher: American Meteorological Society
    Abstract: Snow cover can significantly suppress daytime temperatures by increasing the surface albedo and limiting the surface temperature to 0°C. The strength of this effect is dependent upon how well the snow can cover, or mask, ...
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    Modeling Snow Depth for Improved Simulation of Snow–Vegetation–Atmosphere Interactions 

    Source: Journal of Hydrometeorology:;2004:;Volume( 005 ):;issue: 005:;page 723
    Author(s): Strack, John E.; Liston, Glen E.; Pielke, Roger A.
    Publisher: American Meteorological Society
    Abstract: The presence of snow and its relationship to surrounding vegetation significantly impacts the surface energy balance. For accurate atmospheric model simulations, the degree to which a snowpack can cover vegetation must be ...
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