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    Computer Program for Calculating Average Lengths of Weather Radar Echoes and Pattern Bandedness 

    Source: Journal of the Atmospheric Sciences:;1966:;Volume( 023 ):;issue: 005:;page 569
    Author(s): Kessler, Edwin
    Publisher: American Meteorological Society
    Abstract: The average length of echoes and a measure of pattern bandedness in digitized PPI displays are estimated from exponential-function approximations to the pattern autocorrelation coefficients. Average echo lengths estimated ...
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    Tornadoes 

    Source: Bulletin of the American Meteorological Society:;1970:;volume( 051 ):;issue: 010:;page 926
    Author(s): Kessler, Edwin
    Publisher: American Meteorological Society
    Abstract: The prominent characteristics of tornadoes, their sociological and meteorological importance, aspects of the national weather service that pertain to storm forecasting and warning, observational and theoretical studies of ...
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    Note on Range Normalization of Digitized Radar Data 

    Source: Journal of Applied Meteorology:;1963:;volume( 002 ):;issue: 001:;page 178
    Author(s): Kessler, Edwin
    Publisher: American Meteorological Society
    Abstract: tract
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    ELEMENTARY THEORY OF ASSOCIATIONS BETWEEN ATMOSPHERIC MOTIONS AND DISTRIBUTIONS OF WATER CONTENT 

    Source: Monthly Weather Review:;1963:;volume( 091 ):;issue: 001:;page 13
    Author(s): KESSLER, EDWIN
    Publisher: American Meteorological Society
    Abstract: Continuity equations are used to clarify relationships between air motions and distributions of accompanying precipitation. The equations embody simple modeling of condensation and evaporation with the following assumptions: ...
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    Kinematic Effect of Vertical Drafts on Precipitation near Earth's Surface 

    Source: Monthly Weather Review:;1987:;volume( 115 ):;issue: 011:;page 2862
    Author(s): Kessler, Edwin
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    KINEMATICAL RELATIONS BETWEEN WIND AND PRECIPITATION DISTRIBUTIONS 

    Source: Journal of Meteorology:;1959:;volume( 016 ):;issue: 006:;page 630
    Author(s): Kessler, Edwin
    Publisher: American Meteorological Society
    Abstract: If distributions of precipitation in the atmosphere could be understood in terms of their associated three-dimensional winds, then radar, radiosonde, and surface observations might be utilized in new ways as sources of ...
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    Condensate Content in Relation to Sloping Updraft Parameters 

    Source: Journal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 002:;page 443
    Author(s): Kessler, Edwin
    Publisher: American Meteorological Society
    Abstract: The density of cloud and precipitation relates via simple approximations to the slope, vertical air speed, and diameter of moist updraft columns, and to the fallspeed and residence time of cloud and precipitation particles.
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    KINEMATICAL RELATIONS BETWEEN WIND AND PRECIPITATION DISTRIBUTIONS, II 

    Source: Journal of Meteorology:;1961:;volume( 018 ):;issue: 004:;page 510
    Author(s): Kessler, Edwin
    Publisher: American Meteorological Society
    Abstract: In order to extend our understanding of the relationships between the atmospheric distributions of water substance and the wind, a two-dimensional continuity equation for water substance is studied in terms of model wind ...
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    EYE REGION OF HURRICANE EDNA, 1954 

    Source: Journal of Meteorology:;1958:;volume( 015 ):;issue: 003:;page 264
    Author(s): Kessler, Edwin
    Publisher: American Meteorological Society
    Abstract: The eye region of Hurricane Edna (1954) is studied with the principal aid of radar and dropsonde data. Vertical sections show that over the eye there was a thick layer derived from the wall cloud which bounded the eye on ...
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    Frontal Analysis in the Light of Abrupt Temperature Changes in a Shallow Valley 

    Source: Monthly Weather Review:;1999:;volume( 127 ):;issue: 006:;page 1125
    Author(s): Sanders, Frederick; Kessler, Edwin
    Publisher: American Meteorological Society
    Abstract: The authors examine selected cases of abrupt temperature changes in a shallow valley in rural Oklahoma and examine their wider associations. All changes in the valley, whether rise or fall, are accompanied by a northerly ...
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