Wang, Wei-Chyung and Pinto, Joseph P. and Yung, Yuk Ling (1980) Climatic Effects Due to Halogenated Compounds in the Earth’s Atmosphere. Journal of the Atmospheric Sciences, 37 (2). pp. 333-338. ISSN 0022-4928 http://resolver.caltech.edu/CaltechAUTHORS:20120724-075448222
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Using a one-dimensional radiative-convective model, we perform a sensitivity study of the effect of ozone depletion in the stratosphere on the surface temperature. There could be a cooling of the surface temperature by ~0.2 K due to chlorofluoromethane-induced ozone depletion at steady state (assuming 1973 release rates). This cooling reduces significantly the greenhouse effect due to the presence of chlorofluoromethanes. Carbon tetrafluoride has a strong ν_3 band at 7.8 μm, and the atmospheric greenhouse effect is shown to be 0.07 and 0.12 K (ppbv)^(−1) with and without taking into account overlap with CH_4 and N_2O bands. At concentration higher than 1 ppbv, absorption by the ν_3 band starts to saturate and the greenhouse effect becomes less efficient.
|Additional Information:||© 1980 American Meteorological Society. Manuscript received 4 June 1979, in final form 29 August 1979. We thank N. D. Sze, R. T. Watson, A. Goldman, D. G. Murcray and J. E. Hansen for useful discussion, and R. T. Watson, S. P. Sander and A. A. Lacis for permission to use their results prior to publication. During the course of this work, Pinto was supported by NASA Grant NSG 5163 Scope M to Columbia University. Yung's research was supported by NASA Grant NSG 2229 to the California Institute of Technology.|
|Official Citation:||Wang, Wei-Chyung, Joseph P. Pinto, Yuk Ling Yung, 1980: Climatic Effects Due to Halogenated Compounds in the Earth’s Atmosphere. J. Atmos. Sci., 37, 333–338. doi: http://dx.doi.org/10.1175/1520-0469(1980)037<0333:CEDTHC>2.0.CO;2|
|Usage Policy:||No commercial reproduction, distribution, display or performance rights in this work are provided.|
|Deposited By:||Tony Diaz|
|Deposited On:||26 Jul 2012 23:25|
|Last Modified:||26 Dec 2012 15:42|
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