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    The Radiative Diffusivity Factor for the Random Malkmus Band 

    Source: Journal of the Atmospheric Sciences:;1969:;Volume( 026 ):;issue: 004:;page 741
    Author(s): Armstrong, B. H.
    Publisher: American Meteorological Society
    Abstract: The diffusivity factor r that converts an intensity transmission function to a flux transmission function is calculated for the Lorentz line shape as a function of the optical parameters for the new molecular hand model ...
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    Smoothing of the Intensity Curve Obtained from a Solution of the Spherical Harmonics Approximation to the Transfer Equation 

    Source: Journal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 007:;page 1934
    Author(s): Dave, J. V.; Armstrong, B. H.
    Publisher: American Meteorological Society
    Abstract: Results are presented to show that the quality of the intensity values obtained after solving a spherical harmonics approximation to the transfer equation can be remarkably improved by applying smoothing procedures based ...
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    Operational Responsibilities of the National Weather Service River and Flood Program 

    Source: Weather and Forecasting:;1995:;volume( 010 ):;issue: 003:;page 465
    Author(s): Larson, L.W.; Ferral, R.L.; Strem, E.T.; Morin, A.J.; Armstrong, B.; Carroll, T.R.; Hudlow, M.D.; Wenzel, L.A.; Schaefer, G.L.; Johnson, D.E.
    Publisher: American Meteorological Society
    Abstract: The River and Flood Program in the National Weather Service, in its mission to save lives and property, has the responsibility to gather hydrologic data from a variety of sources and to assemble the data to make timely and ...
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