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The Search for Global CO2 etc. ‘Greenhouse Effects’

Published online by Cambridge University Press:  24 August 2009

Sherwood B. Idso
Sherwood B. Idso
Affiliation:
Research Physicist, US Water Conservation Laboratory, USDA-Agricultural Research Service, 4331 E. Broadway Road, Phoenix, Arizona 85040, USA; Adjunct Professor in the Departments of Geography, Geology, and Botany & Microbiology, Arizona State University, Tempe, Arizona 85287, USA.
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The concentration of carbon dioxide (CO2) in Earth's atmosphere has been steadily increasing since the inception of the Industrial Revolution. Believed to be due primarily to the burning of fossil fuels and the clearing of forests, this phenomenon has two potential consequences of global importance.

Many scientists believe that the CO2 increases projected for Earth's atmosphere by the middle of the next century will lead to a significant warming of the planet which could severely impact world agriculture and cause a melting of polar ice which would greatly raise sea-levels and lead to the flooding of coastal lowlands. Others, however, point to the demonstrable positive effects of elevated concentrations of atmospheric CO2 on plant productivity and wateruse efficiency, suggesting that more CO2 in the air will be beneficial to The Biosphere. Against this backlog of controversy, scientists of both persuasions have attempted the ‘first detection’ of either or both of these effects on a global scale.

With respect to the quest for a climatic ‘signal’, numerous studies conducted to date have come up emptyhanded; it is just not discernible from the natural variations inherent in the data. However, there does appear to be a manifestation of enhanced global photosynthetic activity in the yearly amplitude of atmospheric CO2 concentrations at a number of sites around the world; and the most logical explanation of that seems to be the CO2-induced enhancement of plant growth and development which has been demonstrated to occur in hundreds of laboratory and field experiments.

Type
Main Papers
Information
Environmental Conservation , Volume 12 , Issue 1 , Spring 1985 , pp. 29 - 35
Copyright
Copyright © Foundation for Environmental Conservation 1985

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References

REFERENCES

Angell, J.K. & Korshover, J. (1978 a). Global temperature variation, surface to 100 mb: an update into 1977. Monthly Weather Renew, 106, pp. 755–70.2.0.CO;2>CrossRefGoogle Scholar
Angell, J.K. & Korshover, J. (1978 b). Estimate of global temperature variations in the 100-300 mb layer between 1958 and 1977. Monthly Weather Review, 106, pp. 1422–32.2.0.CO;2>CrossRefGoogle Scholar
Aston, A.R. (1984). The effect of doubling atmospheric CO2 on streamflow: a simulation. Journal of Hydrology, 67, pp. 273–80.CrossRefGoogle Scholar
Bell, T.H. (1982). Optimal weighting of data to detect climatic change: Application to the carbon dioxide problem. Journal of Geophysical Research, 87, pp. 11, 161–76.CrossRefGoogle Scholar
Borzenkova, I.I., Vinnikov, K. Ya., Spirina, L. P. & Stekhnovsky, D.I. (1976). Change in air temperature of the northern hemisphere for the period 1881–1975. Meteorologiya i Gidrologiya, 1, pp. 27–35.Google Scholar
Brewer, P.G. (1978). Direct observation of the oceanic CO2 increase. Geophysical Research Letters, 5, pp. 997–1000.CrossRefGoogle Scholar
Brewer, P.G. (1983). The T.T.O. North Atlantic study—a progress report. Proceedings: Carbon Dioxide Research Conference: Carbon Dioxide, Science and Consensus. US Department of Energy Report CONF-820970, Part II, pp. 91–122.Google Scholar
Callendar, G.S. (1938). The artificial production of carbon dioxide and its influence on temperature. Quarterly Journal of the Royal Meteorological Society, 64, pp. 223–37.CrossRefGoogle Scholar
Callendar, G.S. (1949). Can carbon dioxide influence climate? Weather, 4, pp. 310–4.CrossRefGoogle Scholar
Carbon Dioxide Assessment Committee (1983). Changing Climate. (US National Research Council.) National Academy Press, Washington, DC, USA: xxiii + 496 pp., illustr.Google Scholar
Chiu, L.S. (1983). Variation of Antarctic sea ice: an update. Monthly Weather Review, 111, pp. 578–80.2.0.CO;2>CrossRefGoogle Scholar
Cleveland, W.S., Frenny, A.E. & Graedel, T.E. (1983). The seasonal component of atmospheric CO2: Information from new approaches to the decomposition of seasonal time-series. Journal of Geophysical Research, 88, pp. 10, 934–40, and 946.CrossRefGoogle Scholar
Climate Research Board (1979). Carbon Dioxide and Climate: A Scientific Assessment. (US National Research Council.) National Academy Press, Washington, DC, USA: vi + 22 pp., illustr.Google Scholar
CO2/Climate Review Panel (1982). Carbon Dioxide and Climate: A Second Assessment. (US National Research Council.) National Academy Press, Washington, DC, USA: xx + 72 pp., illustr.Google Scholar
Dalrymple, D.C. (1973). A Global Review of Greenhouse Food Production. US Department of Agriculture, Economic Research Service, Washington, DC, USA: x + 150 pp., illustr.Google Scholar
Dewey, K.R. & Heim, R. Jr (1982). A digital archive of Northern Hemisphere snow-cover, November 1966 through December 1980. Bulletin of the American Meteorological Society, 63, pp. 1132–41.2.0.CO;2>CrossRefGoogle Scholar
Donner, L. & Ramanathan, V. (1980). Methane and nitrous oxide: Their effect on the terrestrial climate. Journal of the Atmospheric Sciences, 37, pp. 119–24.2.0.CO;2>CrossRefGoogle Scholar
Ellsaesser, H.W. (1984). The climatic effect of CO2: a different view. Atmospheric Environment, 18, pp. 431–4.CrossRefGoogle Scholar
Fishman, J., Ramanathan, V., Crutzen, P. & Liu, S. (1979). Tropospheric ozone and climate. Nature (London), 282, pp. 818–20.CrossRefGoogle Scholar
Gifford, R.M. (1979). Growth and yield of CO2-enriched wheat under water-limited conditions. Australian Journal of Plant Physiology, 6, pp. 367–78.Google Scholar
Gilliland, R.L. (1982). Solar, volcanic, and CO2 forcing of recent climate changes. Climatic Change, 4, pp. 111–31.CrossRefGoogle Scholar
Gornitz, V., Lebedeff, S. & Hansen, J. (1982). Global sea-level trend in the past century. Science, 215, pp. 1611–4.CrossRefGoogle ScholarPubMed
Hall, C.A., Edkahl, C.A. & Wartenberg, D.C. (1975). A fifteen-year record of biotic metabolism in the Northern Hemisphere. Nature (London), 255, pp. 136–8.CrossRefGoogle Scholar
Hameed, S., Cess, R. & Hogan, J. (1980). Response of the global climate to changes in atmospheric composition due to fossilfuel burning. Journal of Geophysical Research, 85, pp. 7537–45.CrossRefGoogle Scholar
Hansen, J., Johnson, D., Lacis, A., Lebedeff, S., Lee, P., Rind, D. & Russell, G. (1981). Climate impact of increasing atmospheric carbon dioxide. Science, 213, pp. 957–66.CrossRefGoogle ScholarPubMed
Hummel, J.R. & Reck, R.A. (1981). The direct thermal effect of CHClF2, CH3CCl3 and CH2Cl2 on atmospheric surface temperatures. Atmospheric Environment, 15, pp. 379–82.CrossRefGoogle Scholar
Idso, S.B. (1980). The climatological significance of a doubling of Earth's atmospheric carbon dioxide concentration. Science, 207, pp. 1462–3.CrossRefGoogle ScholarPubMed
Idso, S.B. (1981). Carbon dioxide—an alternative view. New Scientist, 92, pp. 444–6.Google Scholar
Idso, S.B. (1982 a). Carbon Dioxide: Friend or Foe? An Inquiry into the Climatic and Agricultural Consequences of the Rapidly Rising CO2 Content of Earth's Atmosphere. IBR Press, Tempe, Arizona, USA: xiii + 92 pp., illustr.Google Scholar
Idso, S.B. (1982 b). The anthropic principle, Gaia, carbon dioxide, and the human condition. Speculations in Science and Technology, 5, pp. 455–9.Google Scholar
Idso, S.B. (1982 c). Temperature limitation by evaporation in hot climates and the greenhouse effects of water vapor and carbon dioxide. Agricultural Meteorology, 27, pp. 105–9.CrossRefGoogle Scholar
Idso, S.B. (1982d). Long-term stabilization of Earth's surface air temperature by a negative feedback mechanism. Archives for Meteorology, Geophysics and Bioclimatology, Series B, 31, pp. 211–9.CrossRefGoogle Scholar
Idso, S.B. (1982 e). CO2 and climate: Where is the water vapor feedback? Archives for Meteorology, Geophysics and Bioclimatology, Series B, 31, pp. 325–9.CrossRefGoogle Scholar
Idso, S.B. (1982 f). An intriguing climatic observation. Journal de Recherches Atmospheriques, 16, pp. 271–2.Google Scholar
Idso, S.B. (1983 a). Carbon dioxide and global temperature: What the data show. Journal of Environmental Quality, 12, pp. 159–63.CrossRefGoogle Scholar
Idso, S.B. (1983 b). CO2 as an inverse greenhouse gas. Infrared Technology 9, Proceedings of the Society of Photo-Optical Instrumentation Engineers, 430, pp. 232–9.Google Scholar
Idso, S.B. (1983 c). On trusting models or observations. Atmospheric Environment, 17, pp. 1025–6.CrossRefGoogle Scholar
Idso, S.B. (1983 d). Do increases in atmospheric CO2 have a cooling effect on surface air temperature? Climatological Bulletin, 17, pp. 22–6.Google Scholar
Idso, S.B. (1983 e). On the magnitude of the CO2 greenhouse effect. Applied Energy, 14, pp. 227–32.CrossRefGoogle Scholar
Idso, S.B. (1984 a). The case for carbon dioxide. The Journal of Environmental Sciences, 27 (3), pp. 19–22.Google Scholar
Idso, S.B. (1984 b). Shortcomings of CO2-climate models raise questions about the wisdom of energy policy implications. Applied Energy, 16, pp. 53–7.CrossRefGoogle Scholar
Idso, S.B. (1984 c). An empirical evaluation of Earth's surface air temperature response to radiative forcing, including feedback, as applied to the CO2-climate problem. Archives for Meteorology, Geophysics and Bioclimatology, Series B, 34, pp. 1–19.CrossRefGoogle Scholar
Idso, S.B. (1984 d). What if increases in atmospheric CO2 have an inverse greenhouse effect? I: Energy balance considerations related to surface albedo. Journal of Climatology, 4, pp. 399–409.CrossRefGoogle Scholar
Jones, P.D., Wigley, T.M.L. & Kelly, P.M. (1982). Variations in surface air temperatures, Part 1: Northern hemisphere, 1881–1980. Monthly Weather Review, 110, 59–70.2.0.CO;2>CrossRefGoogle Scholar
Kelly, P.M., Jones, P.D., Sear, C.B., Cherry, B.S.G. & Tavakol, R.K. (1982). Variations in surface air temperatures, Part 2: Arctic regions, 1881–1980. Monthly Weather Review, 110, pp. 71–83.2.0.CO;2>CrossRefGoogle Scholar
Kimball, B.A. (1983 a). Carbon dioxide and agricultural yield: an assemblage and analysis of 430 prior observations. Agronomy Journal, 75, pp. 779–88.CrossRefGoogle Scholar
Kimball, B.A. (1983 b). Carbon Dioxide and Agricultural Yield: An Assemblage and Analysis of 770 Prior Observations. US Water Conservation Laboratory, WCL Report 14, Phoenix, Arizona, USA: 71 pp.Google Scholar
Kimball, B.A. & Idso, S.B. (1983). Increasing atmospheric CO2: Effects on crop yield, water use, and climate. Agricultural Water Management, 7, pp. 55–73.CrossRefGoogle Scholar
King, D.A. & Bingham, G.E. (MS). Estimating the Direct Effect of CO2 on Soybean Yield. Unpublished manuscript.*Google Scholar
Lacis, A., Hansen, J., Lee, P., Mitchell, T. & Lebedeff, S. (1981). Greenhouse effect of trace gases. Geophysical Research Letters, 8, pp. 1035–8.CrossRefGoogle Scholar
LaMarche, V.C. Jr, Graybill, D.A., Fritts, H.C. & Rose, M.R. (1984). Increasing atmospheric carbon dioxide: Tree-ring evidence for growth enhancement in natural vegetation. Science, 225, pp. 1019–21.CrossRefGoogle ScholarPubMed
MacCracken, M.C. & Moses, H. (1982). The first detection of carbon dioxide effects: Workshop summary. Bulletin of the American Meteorological Society, 63, pp. 1164–78.Google Scholar
Madden, R.A. & Ramanathan, V. (1980). Detecting climate change due to increasing carbon dioxide. Science, 209, pp. 763–8.CrossRefGoogle ScholarPubMed
Manabe, S. & Wetherald, R.T. (1967). Thermal equilibrium of the atmosphere with a given distribution of relative humidity. Journal of the Atmospheric Sciences, 24, pp. 241–59.2.0.CO;2>CrossRefGoogle Scholar
Manabe, S. & Wetherald, R.T. (1975). The effects of doubling the CO2 concentration on the climate of a general circulation model. Journal of the Atmospheric Sciences, 32, pp. 3–15.2.0.CO;2>CrossRefGoogle Scholar
Matson, M. & Wiesnet, D.R. (1981). New data-base for climate studies. Nature (London), 289, pp. 451–6.CrossRefGoogle Scholar
Namias, J. (1978). Multiple causes of the North American abnormal winter, 1976–77. Monthly Weather Review, 196, pp. 279–95.2.0.CO;2>CrossRefGoogle Scholar
Namias, J. (1980). Some concomitant regional anomalies associated with hemispherically-averaged temperature variations. Journal of Geophysical Research, 85, pp. 1585–90.CrossRefGoogle Scholar
Newell, R.E. & Dopplick, T.G. (1979). Questions concerning the possible influence of anthropogenic CO2 on atmospheric temperature. Journal of Applied Meteorology, 18, pp. 822–5.2.0.CO;2>CrossRefGoogle Scholar
Newell, R.E. & Dopplick, T.G. (1981). Reply to Robert G. Watts' ‘Discussion of «Questions concerning the possible influence of anthropogenic CO2 on atmospheric temperature ».’ Journal of Applied Meteorology, 20, pp. 114–7.2.0.CO;2>CrossRefGoogle Scholar
Pearman, G.T. & Hyson, P. (1981). The annual variation of atmospheric CO2 concentration observed in the northern hemisphere. Journal of Geophysical Research, 86, pp. 9839–43.CrossRefGoogle Scholar
Plass, G.N. (1956). Effect of carbon dioxide variations on climate. American Journal of Physics, 24, pp. 376–87.CrossRefGoogle Scholar
Ramanathan, V. (1975). Greenhouse effect due to chlorofluoro-carbons: Climatic implications. Science, 190, pp. 50–1.CrossRefGoogle Scholar
Raper, S.C.B., Wigley, T.M.L., Jones, P.D., Kelly, P.M., Mayes, P.R. & Limbert, D.W.S. (1983). Recent temperature changes in the Arctic and Antarctic. Nature (London), 306, pp. 458–9.CrossRefGoogle Scholar
Revelle, R. (1982). Carbon dioxide and world climate. Scientific American, 247 (2), pp. 35–43.CrossRefGoogle Scholar
Rogers, H.H., Thomas, J.F. & Bingham, G.E. (1983). Response of agronomic and forest species to elevated atmospheric carbon dioxide. Science, 220, pp. 428–9.CrossRefGoogle ScholarPubMed
Schneider, S.H. (1983). The problem of ‘pre-industrial’ CO2 concentration — an editorial. Climatic Change, 5, pp. 311–3.CrossRefGoogle Scholar
Schonwiese, C.-D. (1983). Northern hemisphere temperature statistics and forcing, Part A: 1881–1981 AD. Archives for Meteorology, Geophysics and Bioclimatology, Series B, 32, pp. 337–60.CrossRefGoogle Scholar
Seidel, S. & Keyes, D. (1983). Can We Delay a Greenhouse Warming? US Environmental Protection Agency, Washington, DC, USA: ix + 188 pp., illustr.Google Scholar
Stanhill, G. (1983). Reply with some additional details on ‘the Montsouris series of carbon dioxide concentration measurements, 1877–1910.’ Climatic Change, 5, pp. 417–9.CrossRefGoogle Scholar
Thompson, S.L. & Schneider, S.H. (1982). Carbon dioxide and climate: Has a signal been observed yet? Nature (London), 295, pp. 645–6.CrossRefGoogle Scholar
Tolbert, N.E. & Zelitch, I. (1983). Carbon metabolism. Pp. 21–64 in CO2 and Plants (Ed. Lemon, E.R.). Westview Press, Boulder, Colorado, USA: xxii + 280 pp., illustr.Google Scholar
Tyndall, J. (1861). On the absorption and radiation of heat by gases and vapours, and on the physical connection of radiation, absorption, and conduction. Philosophical Magazine Series, 4 (22), pp. 169–94 and 273–85.CrossRefGoogle Scholar
Vinnikov, K. Ya. & Groisman, P. Ya. (1981). An empirical analysis of the influence of CO2 on contemporary variations in annual average surface air temperature in the northern hemisphere. Meteorologiya i Gidrologiya, 11, pp. 30–43.Google Scholar
Wang, W.C., Yung, Y., Lacis, A., Mo, T. & Hansen, J. (1976). Greenhouse effects due to Man-made perturbations of trace gases. Science, 194, pp. 685–90.CrossRefGoogle Scholar
Wang, W., Pinto, J.P. & Yung, Y.L. (1980). Climatic effects due to halogenated compounds in the Earth's atmosphere. Journal of the Atmospheric Sciences, 37, pp. 333–8.2.0.CO;2>CrossRefGoogle Scholar
Wigley, T.M.L. (1983). The pre-industrial carbon dioxide level. Climatic Change, 5, pp. 315–20.CrossRefGoogle Scholar
Wigley, T.M.L. & Jones, P.D. (1981). Detecting CO2-induced climatic change. Nature (London), 292, pp. 205–8.CrossRefGoogle Scholar
Wigley, T.M.L., Jones, P.D. & Kelly, P.M. (1981). Global warming? Nature (London), 291, p. 285.CrossRefGoogle Scholar
Wittwer, S.H. (1982). Carbon dioxide and crop productivity. New Scientist, 95, pp. 233–4.Google Scholar
Wittwer, S.H. & Robb, W. (1964). Carbon dioxide enrichment of greenhouse atmospheres for food-crop production. Economic Botany, 18, pp. 34–56.CrossRefGoogle Scholar
Yamamoto, R. & Hoshiai, M. (1979). Recent change of the northern hemisphere mean surface air temperature estimated by optimal interpolation. Monthly Weather Review, 107, pp. 1239–44.2.0.CO;2>CrossRefGoogle Scholar
Zwally, H.J., Parkinson, C.L. & Comiso, J.C. (1983). Variability of Antarctic sea-ice and changes in carbon dioxide. Science, 220, pp. 1005–12.CrossRefGoogle ScholarPubMed