According to the simplest model of the earth’s radiative balance, global warming will occur with certainty as humankind increases its production and consumption of nonsolar energy. This prediction is revisited, using a broader model that allows the greenhouse effect to be considered. The new model predicts a global warming of where ε is the rate of surface energy release in units of the average incident solar radiation, and is the average temperature rise at the earth’s surface. Present values of these quantities, excluding geothermal sources, are and The model assigns a small number of optical parameters to the atmosphere and surface and qualifies the simple warming prediction: It is rigorous only if parameters other than ε are unchanged. The model is not complex and should serve as an aid to an elementary understanding of global warming.
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December 1999
PAPERS|
December 01 1999
Physical aspects of the greenhouse effect and global warming
Special Collection:
Teaching about the environment, sustainability, and climate change (1975-2022)
Robert S. Knox
Robert S. Knox
Laboratory for Laser Energetics, University of Rochester, Rochester, New York 14623-1299
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Am. J. Phys. 67, 1227–1238 (1999)
Article history
Received:
March 12 1999
Accepted:
June 11 1999
Citation
Robert S. Knox; Physical aspects of the greenhouse effect and global warming. Am. J. Phys. 1 December 1999; 67 (12): 1227–1238. https://doi.org/10.1119/1.19109
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