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change in low clouds with the change in global temperature. The factor of 0.25 +/- 0.18 W/m2/K, when expressed in these units rather than % cloud fraction/K. x_i are the above clouds stabilizing factors. Figure 2b shows how the feedback produce when changes in five of these six factors are taken from AOGCMs combined with the information from large eddy simulation models to calculate the feedback from low tropical clouds. Warmer SSTs produced a local feedback of nearly Amazing st patricks day irish celtic full printing bedding set + 2 W/m2/K in LES. The strengthened inversion stability predicted by AOGCMs was expected produces a local feedback of about -1 W/m2/K in LES models. The other factors have negligible impact. However, we can’t be sure that climate model with their lousy clouds (only half as many low clouds as observed off

 

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