CALCULATION OF ATMOSPHERIC RADIATIVE FORCING (WARMING EFFECT) OF CARBON DIOXIDE AT ANY CONCENTRATION* by H. Douglas Lightfoot and Orval A. Mamer (Canada) November 8, 2014 Summary for wide circulation This is a scientific paper and such papers are often not readily understood beyond the scientific community. Because the results of this paper are important to the present debate about carbon dioxide emissions, this short summary is prepared for much wider circulation. Carbon dioxide (CO2) is a warming gas because it captures infrared heat radiation (IR) from the earth and warms the air surrounding it. At a given concentration of CO2, a certain amount of the available IR is absorbed by the CO2. If more CO2 is added, the warming effect of the added CO2 is less per molecule because some of the IR has already been absorbed. At some point, further additions of CO2 will have no warming effect because all of the available IR will have been absorbed Currently, there is general agreement that the relationship between warming and concentration is a logarithm curve, a mathematical curve with a characteristic shape. This curve works well within the current concentration range of interest of 275 in 1750 to 378 parts per million by volume (ppmv) in 2005. Problems beyond this range limit its usefulness. For example, it does not start at zero and, therefore, does not give actual warming measurements, but only the difference between two concentrations. There are no limits as to where the logarithmic curve is valid and where it is not, and there is no upper limit because the curve continues upwards indefinitely. To resolve these problems, by trial and error we found a quadratic curve, which has a different characteristic shape from that of the logarithm. It exactly matches the logarithm curve over the range of 275 to 378 ppmv, starts at zero and reaches a limit where the curve becomes horizontal. The fact that the curve starts at zero establishes the warming effect at 378 ppmv as 8.67 watts per square metre (W m-2). The upper limit of concentration where the curve becomes horizontal is calculated exactly by calculus at 654.6 ppmv. We also found a sine curve, which has different characteristic shape again, that does the same as the quadratic, but with a warming effect at 378 ppmv of 7.48 W m-2. Any mathematical curve that meets the restrictions will have warming values close to 8.67 or 7.48 W m-2. *From: ENERGY & ENVIRONMENT, VOLUME 25, NOV 8, 2014, MULTI-SCIENCE PUBLISHING COMPANY LTD 1