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    A Quasi-Three-Dimensional Climate Model 

    Source: Journal of Climate and Applied Meteorology:;1983:;volume( 022 ):;issue: 009:;page 1557
    Author(s): Sellers, William D.
    Publisher: American Meteorological Society
    Abstract: A quasi-three-dimensional global climate model designed to trace the transient evolution of climate is described. The model, which has an interactive ocean, differs from earlier models in including a 5-layer atmospheric ...
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    Potential Evapotranspiration in Arid Regions 

    Source: Journal of Applied Meteorology:;1964:;volume( 003 ):;issue: 001:;page 98
    Author(s): Sellers, William D.
    Publisher: American Meteorological Society
    Abstract: The concept of potential evapotranspiration, as applied to arid regions, is examined using an energy balance approach suggested by Budyko. Using data for Yuma, Ariz., it is shown that a 50 per cent increase in the relative ...
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    CLIMATOLOGY OF MONTHLY PRECIPITATION PATTERNS IN THE WESTERN UNITED STATES, 1931–1966 

    Source: Monthly Weather Review:;1968:;volume( 096 ):;issue: 009:;page 585
    Author(s): SELLERS, WILLIAM D.
    Publisher: American Meteorological Society
    Abstract: The eigenvector or ?empirical orthogonal function? approach is used to determine the dominant precipitation anomaly patterns for the western United States for each month during the last 36 yr. In all months there is enough ...
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    A Two–Dimensional Global Climatic Model 

    Source: Monthly Weather Review:;1976:;volume( 104 ):;issue: 003:;page 233
    Author(s): Sellers, William D.
    Publisher: American Meteorological Society
    Abstract: A two?dimensional global climatic model has been developed, using a 10° longitude by 10° latitude box grid and a one-month time step. The lapse rates of temperature and the meridional component of the flow in the oceans ...
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    A New Global Climatic Model 

    Source: Journal of Applied Meteorology:;1973:;volume( 012 ):;issue: 002:;page 241
    Author(s): Sellers, William D.
    Publisher: American Meteorological Society
    Abstract: A global climatic model, allowing for seasonal coupling and interaction between continents and oceans, is developed, utilizing an idealized land-water distribution similar to that observed. The basic equation used is the ...
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    The Effect of Changes in the Earth's Obliquity on the Distribution of Mean Annual Sea-Level Temperatures 

    Source: Journal of Applied Meteorology:;1970:;volume( 009 ):;issue: 006:;page 960
    Author(s): Sellers, William D.
    Publisher: American Meteorological Society
    Abstract: tract
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    Reply 

    Source: Journal of Applied Meteorology:;1970:;volume( 009 ):;issue: 002:;page 311
    Author(s): Sellers, William D.
    Publisher: American Meteorological Society
    Abstract: tract
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    A Global Climatic Model Based on the Energy Balance of the Earth-Atmosphere System 

    Source: Journal of Applied Meteorology:;1969:;volume( 008 ):;issue: 003:;page 392
    Author(s): Sellers, William D.
    Publisher: American Meteorological Society
    Abstract: A relatively simple numerical model of the energy balance of the earth-atmosphere is set up and applied. The dependent variable is the average annual sea level temperature in 10° latitude belts. This is expressed basically ...
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    A STATISTICAL METHOD FOR ESTIMATING THE MEAN RELATIVE HUMIDITY FROM THE MEAN AIR TEMPERATURE 

    Source: Monthly Weather Review:;1960:;volume( 088 ):;issue: 004:;page 155
    Author(s): SELLERS, WILLIAM D.
    Publisher: American Meteorological Society
    Abstract: This paper outlines a method of estimating the mean relative humidity from the mean temperature. Ordinary linear regression techniques are used, with a correction added to account for the systematic geographical distribution ...
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    A Reassessment of the Effect of CO2 Variations on a Simple Global Climatic Model 

    Source: Journal of Applied Meteorology:;1974:;volume( 013 ):;issue: 007:;page 831
    Author(s): Sellers, William D.
    Publisher: American Meteorological Society
    Abstract: A simple global climatic model described earlier is modified slightly and reapplied to the CO2 problem. The modifications include using a more efficient numerical method to solve the system of equations and changing the ...
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