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Super greenhouse effect

Inamdar and Ramanathan (1998) have shown that there are considerable geographical variations in water vapor feedback, with the dominating effect in the ec]uatorial ocean region. In this area the greenhouse feedback exceeds the blackbody emission, reproducing the so-called super-greenhouse effect (Ramanathan and Collins, 1991). The overall results demonstrate the importance of realistically reproducing the three-dimensional atmospheric circulation and the associated water distribution for a credible water vapor feedback. [Pg.21]


See other pages where Super greenhouse effect is mentioned: [Pg.492]    [Pg.278]    [Pg.492]    [Pg.278]    [Pg.194]    [Pg.265]    [Pg.69]    [Pg.552]    [Pg.5]   
See also in sourсe #XX -- [ Pg.21 ]




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Greenhouse effect

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