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Plass, Gilbert N. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
The most recent calculations of the infra-red flux in the region of the 15 micron CO2 band show that the average surface temperature of the earth increases 3.6° C if the CO2 concentration in the atmosphere is doubled and decreases 3.8° C if the CO2 amount is halved, provided that no other factors change which influence the radiation balance. Variations in CO2 amount of this magnitude must have occurred during geological history; the resulting temperature changes were sufficiently large to influence the climate. The CO2 balance is discussed. The CO2 equilibrium between atmosphere and oceans is calculated with and without CaCO3 equilibrium, assuming that the average temperature changes with the CO2 concentration by the amount predicted by the CO2 theory. When the total CO2 is reduced below a critical value, it is found that the climate continuously oscillates between a glacial and an inter-glacial stage with a period of tens of thousands of years; there is no possible stable state for the climate. Simple explanations are provided by the CO2 theory for the increased precipitation at the onset of a glacial period, the time lag of millions of years between periods of mountain building and the ensuing glaciation, and the severe glaciation at the end of the Carboniferous. The extra CO2 released into the atmosphere by industrial processes and other human activities may have caused the temperature rise during the present century. In contrast with other theories of climate, the CO2 theory predicts that this warming trend will continue, at least for several centuries.DOI: 10.1111/j.2153-3490.1956.tb01206.x
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    • ARRHENIUS.,, 1896: O n the influence of carbonic acid in the air upon the temperature of the ground. Phil. Mag. 41, 237-276.
    • BROOKSC, . E. P., 1951: Geological and historical aspects of climatic change. Comp. of Meteor., Boston, Mass. p. 1004-1018.
    • CALLENDAGR., S., 1938: The artificial production of carbon dioxide and its influence on temperature. Quart. J. R o y . Met. Soc., 64, 223-237.
    • - 1949: Can carbon dioxide influence climate? Weather, 4. 310-314.
    • CHAMBERLITN. ,C., 1897,1898,1899:A group of hypotheses bearing on climatic changes.-J. L$ Geology 5 , 653-683; The influence of great epochs of limestone formation upon the constitution of the atmosphere. J. of Geology 6, 609-621; An attempt to frame a working hypothesis of the cause of glacial periods on an atmospheric basis. J. of Geology 7 , 545-584; 667-685; 751-787.
    • CLOUDW,. H., 1952: The 15 micron band of CO, broadened by nitrogen and helium. O N R Progress Report, Johns Hopkins Univ., Baltimore.
    • DINGLE,A. N., 1954: (The carbon dioxide exchange between the North Atlantic Ocean and the atmosphere. Tellus 6, 342-350.
    • ELSASSERW, . M., 1942: Heat transfer by infrared radiation in the atmosphere. Cambridge, Harvard Univ. Press, 107 P.
    • FLINT, R. F., 1947: Glacial geology and the pliestocene epoch. N e w York, John Wiley and Sons, p. 589.
    • FOURIER, M., 1827: Memoire sur les temperatures du globe terrestre et des espaces planktaires. Mem. de I'AcadPmie Royale des Sciences de Z'lnstitut de France 7 , 569-604.
    • KULPJ,. L., 1952: The carbon 1 4 method of age determination. Scientific Monthly 75, 259-267.
    • PLASSG,. N., 1953:The carbon dioxide theory of climatic change. Trans. Amer. Geophysical Union 34, 332; Bull. Amer. Met. SOC.34, 80.
    • - 1956 a: T h e influence of the 9.6 micron ozone band on the atmospheric infra-red cooling rate. Quart. J . R o y . Met. SOC.82, pp. 30-44.
    • - 1956b: The influence of the 1 5 micron carbon dioxide band on the atmospheric infra-red cooling rate. Quart. J . Roy. Met. Soc. (in press).
    • PLASS,G. N., and FIVEL,D. I., 1955 a: A method for the integration of the radiative-transfer equation. J . Met. 12, 191-200.
    • - 1955 b: The influence of variable mixing ratio and temperature on the radiation flux. Quart. J . Roy. Met. Soc. 81,4 8 - 6 2 .
    • RUBEY,W. W., 1951: Geologic history of sea water. Geol. Soc. Amer., Bull., 62, 1111-1148.
    • SHAPLEY,H., editor, 1953: Climatic change: evidence. causes, and efects. Cambridge, Harvard Univ. Press, 318 P.
    • SMITH,C. L., 1940:The Great Bahama Bank. 11. Calcium carbonate precipitation. Jour. Marine Research 3. I 71-1 89.
    • SVERDBUPH,. U.,JOHNSON, M. W . , and FLEMING, R. H., 1942: The oceans: their physics, chemistry, and general biology. New York, Prentice-Hall, 1087p.
    • TYNDALJL.,, 1861:O n the absorption and radiation of heat by gases and vapours. and on the physical connection of radiation, absorption, and conduction. Phil. Mag. 22 (Series 4), 169-194; 273-285.
    • UREYH,. C., 1952: The planets: their origin and development. New Haven, Yale University Press, 245 p.
    • WILLETTH,.C.,1949: Long-period fluctuations of the general circulation of the atmosphere. J. M e t . 6 , 34-50.
    • WISEMAJN.D, H.., 1954: The determination and significance of past temperature changes in the upper layer of the equatorial Azlantic Ocean. Proc. Roy. SOC. London A 222, 296-323.
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