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    Mesoscale Association of a Low-level Jet Stream with a Squall-Line—Cold-Front Situation 

    Source: Journal of Applied Meteorology:;1963:;volume( 002 ):;issue: 001:;page 49
    Author(s): Gerhardt, J. R.
    Publisher: American Meteorological Society
    Abstract: Wind and temperatures data taken at twelve levels on a television tower near Dallas, Tex., are examined during a squall-line?cold-front situation occurring during the morning hours of 8 May 1961. The observations, supplemented ...
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    AN EXAMPLE OF A NOCTURNAL LOW-LEVEL JET STREAM 

    Source: Journal of the Atmospheric Sciences:;1962:;Volume( 019 ):;issue: 001:;page 116
    Author(s): Gerhardt, J. R.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    ON A NEW METHOD OR THE STUDY OF ATMOSPHERIC TURBULENCE NEAR THE EARTH'S SURFACE 

    Source: Journal of Meteorology:;1951:;volume( 008 ):;issue: 005:;page 363
    Author(s): Crain, C. M.; Gerhardt, J. R.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    SURFACE ATMOSPHERIC HEAT-FLUX ANALYSIS ON THE LETTAU MODEL 

    Source: Journal of Meteorology:;1953:;volume( 010 ):;issue: 001:;page 10
    Author(s): Jehn, K. H.; Gerhardt, J. R.
    Publisher: American Meteorological Society
    Abstract: Determinations of the turbulent flux of heat at the earth's surface are made for the period 24?25 January 1950 at Manor, Texas, with use of mean vertical gradients of air temperature and wind speed, following the Lettau ...
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    A PRELIMINARY STUDY OF THE EDDY TRANSFER OF HEAT NEAR THE EARTH'S SURFACE 

    Source: Journal of Meteorology:;1950:;volume( 007 ):;issue: 005:;page 343
    Author(s): Jehn, K. H.; Gerhardt, J. R.
    Publisher: American Meteorological Society
    Abstract: Preliminary time- and height-distributions of the coefficient of eddy conductivity (KH) are presented for three different 24-hour periods for locations in east-central Texas and southern Arizona. It was found that daytime ...
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    ABSORPTION CROSS-SECTIONS OF WATER DROPS FOR INFRARED RADIATION 

    Source: Journal of Meteorology:;1961:;volume( 018 ):;issue: 006:;page 818
    Author(s): Stephens, J. J.; Gerhardt, J. R.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available.
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    FLUCTUATIONS OF ATMOSPHERIC TEMPERATURE AS A MEASURE OF THE SCALE AND INTENSITY OF TURBULENCE NEAR THE EARTH'S SURFACE 

    Source: Journal of Meteorology:;1952:;volume( 009 ):;issue: 005:;page 299
    Author(s): Gerhardt, J. R.; Crain, C. M.; Smith, H. W.
    Publisher: American Meteorological Society
    Abstract: This study summarizes certain preliminary observations on the structure of turbulence near the earth's surface. An array of sensitive bead thermistors is used to measure temperature or temperature-difference fluctuations ...
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    FURTHER STUDIES OF THE BACK-SCATTERING CROSS-SECTIONS OF WATER DROPS AND WET AND DRY ICE SPHERES 

    Source: Journal of Meteorology:;1961:;volume( 018 ):;issue: 005:;page 688
    Author(s): Gerhardt, J. R.; Tolbert, C. W.; Brunstein, S. A.
    Publisher: American Meteorological Society
    Abstract: By using laboratory techniques described in a previous paper, results of the measurements of the back-scattering cross-sections of falling water drops and suspended ice spheres are presented for wavelengths of 1.50 and ...
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    EXPERIMENTAL DETERMINATIONS OF THE BACK-SCATTERING CROSS-SECTIONS OF WATER DROPS AND OF WET AND DRY ICE SPHERES AT 3.2 CENTIMETERS 

    Source: Journal of Meteorology:;1961:;volume( 018 ):;issue: 003:;page 340
    Author(s): Gerhardt, J. R.; Tolbert, C. W.; Brunstein, S. A.; Bahn, W. W.
    Publisher: American Meteorological Society
    Abstract: Measurements are presented of the back-scattering cross-sections of individual water drops and ice pellets at a wavelength of 3.2 cm which cover a diameter range of about 2 to 7 mm for water and 3 to 35 mm for ice. The ...
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