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    Prediction of Cooling of a Nocturnal Environment Using Two Atmospheric Models 

    Source: Journal of Applied Meteorology:;1988:;volume( 027 ):;issue: 004:;page 473
    Author(s): Heinemann, Paul H.; Martsolf, J. David
    Publisher: American Meteorological Society
    Abstract: A surface energy balance model and a boundary layer model were used to predict nocturnal cooling in an agricultural environment. The results from both models were compared with the observed temperatures to determine which ...
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    Spray Irrigation Effects on Surface-Layer Stability in an Experimental Citrus Orchard during Winter Freezes 

    Source: Journal of Applied Meteorology:;1997:;volume( 036 ):;issue: 002:;page 155
    Author(s): Cooper, Harry J.; Smith, Eric A.; Martsolf, J. David
    Publisher: American Meteorological Society
    Abstract: Observations taken by two surface radiation and energy budget stations deployed in the University of Florida/Institute for Food and Agricultural Service experimental citrus orchard in Gainesville, Florida, have been analyzed ...
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    Combination of Manually Digitized Radar and GOES IR for Real-Time Display of Rainfall Intensity 

    Source: Journal of Climate and Applied Meteorology:;1987:;Volume( 026 ):;Issue: 008:;page 1046
    Author(s): Heinemann, Paul H.; Martsolf, J. David; Gerber, John F.; Smith, Daniel L.
    Publisher: American Meteorological Society
    Abstract: Manually Digitized Radar (MDR) and Geostationary Operational Environmental Satellite (GOES) thermal infrared (IR) data were merged to form a higher-resolution radar/IR product than that represented by the MDR. The combination ...
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    Horizontal Coherence Decay Near Large Mesoscale Variations in Topography 

    Source: Journal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 010:;page 1884
    Author(s): Perry, Steven G.; Norman, John M.; Panofsky, Hans A.; Martsolf, J. David
    Publisher: American Meteorological Society
    Abstract: A surface layer experiment is described which includes measurements of turbulent velocities at 2 m above the surface with an army of newly developed drag anemometers. The experiment site is located in central Pennsylvania ...
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