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Greenhouse gases absorbance spectra

After water vapor and C02, methane (CH4) is the third most important greenhouse gas. Each additional molecule of CH4 added to the atmosphere absorbs about 20 times as much long-wave infrared radiation as does a molecule of carbon dioxide. This occurs in part because some of the absorption spectrum of methane lies in windows in the carbon dioxide absorption spectrum (see Fig. 4-42) therefore, methane absorbs wavelengths that are not already being highly attenuated by carbon dioxide. Currently, the global concentration of methane in the atmosphere is approximately 1.7 ppm and is increasing at an annual rate of approximately 0.01 ppm per year (Table 4-14). The seasonal fluctuations shown in Fig. 4-44 may correspond to seasonal... [Pg.390]


See other pages where Greenhouse gases absorbance spectra is mentioned: [Pg.111]    [Pg.212]    [Pg.258]    [Pg.1055]    [Pg.1113]    [Pg.7168]    [Pg.185]    [Pg.500]    [Pg.215]    [Pg.418]    [Pg.425]    [Pg.1224]    [Pg.156]    [Pg.121]   
See also in sourсe #XX -- [ Pg.420 , Pg.422 ]




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