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The infrared strengths of three vibrational band systems of halocarbon F‐11 and four vibrational band systems of halocarbon F‐12 in the ‘atmospheric window’ between 8 and 16 μm were measured at 296±1 K using a Fourier transform infrared spectrometer. These results were obtained at a maximum instrumental resolution of 0.06 cm −1 Our measurements of the total infrared band strengths for F‐11 and F‐12 would indicate approximately 17% and 5% greater absorbance, respectively, than those strengths used in recent greenhouse warming calculations by Ramanathan (1975), Wang et al. (1976), and Lacis et al. (1981), and consequently, a corresponding increase in the possible atmospheric warming effect by these halocarbons.
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Kagann et al. (1983) studied this question.
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