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    A Solution of the Nonlinear Vorticity Equation for Atmospheric Motion 

    Source: Journal of Meteorology:;1945:;volume( 002 ):;issue: 003:;page 175
    Author(s): Craig, Richard A.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    The Vorticity Budget of the Wintertime Lower Stratosphere1 

    Source: Journal of the Atmospheric Sciences:;1967:;Volume( 024 ):;issue: 005:;page 558
    Author(s): Craig, Richard A.
    Publisher: American Meteorological Society
    Abstract: Terms in the vorticity equation are approximated numerically for each of a act of grid points, map times and pressure levels in the lower stratosphere during January-February 1957. The hypothesis is advanced that the ...
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    A Simple Model for the Vertical Distribution of Ozone 

    Source: Journal of Applied Meteorology:;1971:;volume( 010 ):;issue: 005:;page 1046
    Author(s): Craig, Richard A.
    Publisher: American Meteorological Society
    Abstract: tract
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    SURFACE-PRESSURE VARIATIONS FOLLOWING GEOMAGNETICALLY DISTURBED AND GEOMAGNETICALLY QUIET DAYS 

    Source: Journal of Meteorology:;1952:;volume( 009 ):;issue: 002:;page 126
    Author(s): Craig, Richard A.
    Publisher: American Meteorological Society
    Abstract: The average surface-pressure variations after geomagnetically disturbed and geomagnetically quiet days are studied at various locations in a network covering the northern hemisphere between 30 and 70°N. For the same location ...
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    Adoption of Systemè International (SI) Units in AMS Publications 

    Source: Journal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 008:;page 1957
    Author(s): Craig, Richard A.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Umkehr Measurements at Tallahassee 

    Source: Journal of Applied Meteorology:;1976:;volume( 015 ):;issue: 005:;page 509
    Author(s): Craig, Richard A.
    Publisher: American Meteorological Society
    Abstract: For a sample of 59 Umkehr measurements at Tallahassee, the N values are positively correlated with total amount of ozone at all zenith angles, and the normalized N values are positively correlated with the total amounts ...
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    New Editorial Procedures for the Journal of the Atmospheric Sciences 

    Source: Journal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 002:;page 220
    Author(s): Craig, Richard A.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    A Note on the Transmissivity of an Elsasser Band 

    Source: Journal of the Atmospheric Sciences:;1963:;Volume( 020 ):;issue: 001:;page 66
    Author(s): Craig, Richard A.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    VERTICAL EDDY TRANSFER OF HEAT AND WATER VAPOR IN STABLE AIR 

    Source: Journal of Meteorology:;1949:;volume( 006 ):;issue: 002:;page 123
    Author(s): Craig, Richard A.
    Publisher: American Meteorological Society
    Abstract: Detailed soundings of temperature and humidity between the surface and 1000 ft in warm air moving over cooler water are studied to determine the vertical transfer of heat and water vapor due to turbulence. Under simplifying ...
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    THE TEMPERATURE DEPENDENCE OF OZONE RADIATIONAL HEATING RATES IN THE VICINITY OF THE MESOPEAK 

    Source: Journal of Meteorology:;1958:;volume( 015 ):;issue: 001:;page 59
    Author(s): Craig, Richard A.; Ohring, George
    Publisher: American Meteorological Society
    Abstract: Radiational heating of the mesosphere results principally from absorption of ultraviolet radiation by ozone. For conditions of photochemical equilibrium, the amount of ozone present near the mesopeak depends critically on ...
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