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contributor authorShine, Keith P.
date accessioned2017-06-09T14:30:26Z
date available2017-06-09T14:30:26Z
date copyright1991/06/01
date issued1991
identifier issn0022-4928
identifier otherams-20555.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4156796
description abstractThis note examines some of the factors important in determining the large radiative impact, relative to carbon dioxide, of increased concentrations of gases in the optically thin limit (such as the halocarbons at their present day concentrations). A narrow-band radiative transfer model is used to show that an absorber with the same integrated band strength as CFC-12, but with almost the same spectral variation of tropopause net flux change as occurs for small variations in carbon dioxide concentration, is 400 times more effective than carbon dioxide, on a molecule-per-molecule basis; this can be compared with the relative strength of 20 000 for CFC-12. This illustrates that the dominant reason for the relative strength of such gases is not their position in the 8?13 ?m window. It is not possible to unambiguously separate the possible reasons (spectral position, preexisting amounts and spectroscopic strength) for the variations in relative strength, as they are all related.
publisherAmerican Meteorological Society
titleOn the Cause of the Relative Greenhouse Strength of Gases such as the Halocarbons
typeJournal Paper
journal volume48
journal issue12
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1991)048<1513:OTCOTR>2.0.CO;2
journal fristpage1513
journal lastpage1518
treeJournal of the Atmospheric Sciences:;1991:;Volume( 048 ):;issue: 012
contenttypeFulltext


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