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    The “Greenhouse” Effect 

    Source: Journal of Applied Meteorology:;1973:;volume( 012 ):;issue: 003:;page 556
    Author(s): Lee, R.
    Publisher: American Meteorological Society
    Abstract: tract
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    Planetary Boundary Layer Winds in Baroclinic Conditions 

    Source: Journal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 004:;page 1003
    Author(s): Hoxit, Lee R.
    Publisher: American Meteorological Society
    Abstract: Systematic stratifications and analyses of low-level radiosonde data are performed for portions of the eastern half of the United States. The procedures are designed to specify changes in the planetary boundary layer wind ...
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    AN IMPROVED ELECTRONIC DEW-POINT HYGROMETER 

    Source: Journal of Meteorology:;1951:;volume( 008 ):;issue: 001:;page 40
    Author(s): Barrett, Earl W.; Herndon, Lee R.
    Publisher: American Meteorological Society
    Abstract: After a theoretical discussion of the basic physical principles involved in the dew-point method of hygrometry, which serves to establish the inherent advantages of the technique, the paper describes the operating principles ...
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    Diurnal and Annual Temperature Variations in the 30—60 km Region as Indicated by Statistical Analysis of Rocketsonde Temperature Data 

    Source: Journal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 005:;page 922
    Author(s): Hoxit, Lee R.; Henry, Robert M.
    Publisher: American Meteorological Society
    Abstract: Rocketsonde temperature data taken during the period 1964?69 at White Sands, N. M., Cape Kennedy, Fla., and Wallops Island, Va., are stratified into 10 day and 10 night intervals and then averaged to give mean diurnal ...
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    A Short Method of Generating Meteorological Fields for Simulation Studies 

    Source: Journal of Applied Meteorology:;1979:;volume( 018 ):;issue: 012:;page 1670
    Author(s): Pratte, J. F.; Lee, R. W.
    Publisher: American Meteorological Society
    Abstract: We present a computationally convenient method whereby system designers can generate multidimensional meteorological fields for simulation modeling. The procedure, based in digital filtering, efficiently produces large ...
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    Linearized Calculations of Urban Heat Island Convection Effects 

    Source: Journal of the Atmospheric Sciences:;1971:;Volume( 028 ):;issue: 008:;page 1374
    Author(s): Olfe, D. B.; Lee, R. L.
    Publisher: American Meteorological Society
    Abstract: Steady, linearized flow calculations are carried out to estimate vertical temperature profiles over a heated area representing a city. Initially, planar flow is considered in a stable atmosphere with a constant stability ...
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    Airborne Doppler Lidar Wind Field Measurements 

    Source: Bulletin of the American Meteorological Society:;1984:;volume( 065 ):;issue: 004:;page 348
    Author(s): Bilbro, J.; Fichtl, G.; Fitzjarrald, D.; Krause, M.; Lee, R.
    Publisher: American Meteorological Society
    Abstract: A coherent Doppler lidar has been used in an aircraft to measure the 2-dimensional wind field in a number of different atmospheric situations. The lidar, a pulsed CO2 system, was installed in the NASA Convair 990. Galileo ...
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    Reply 

    Source: Monthly Weather Review:;1978:;volume( 106 ):;issue: 007:;page 1034
    Author(s): Hoxit, Lee R.; Fritsch, J. Michael; Chappell, Charles F.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Reply and Corrigendum 

    Source: Monthly Weather Review:;1977:;volume( 105 ):;issue: 008:;page 1063
    Author(s): Hoxit, Lee R.; Chappell, Charles F.; Fritsch, J. Michael
    Publisher: American Meteorological Society
    Abstract: Correction to Volume 104, Issue 11, Article 1408.
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    Variability of SO=4, Total Sulfate, NO−3, and Total Nitrate Scavenging Ratios for the Frontal Boundary Study 

    Source: Journal of Applied Meteorology:;1997:;volume( 036 ):;issue: 006:;page 792
    Author(s): Davis, W. E.; Thorp, J. M.; Lee, R. N.
    Publisher: American Meteorological Society
    Abstract: Precipitation and air concentration data collected during a U.S. Department of Energy?sponsored Frontal Boundary Study (FBS) were used to calculate scavenging ratios. The precipitation data were collected on a 100 km ? 100 ...
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