Skip to main content
. 2009 Dec 22;107(2):571–575. doi: 10.1073/pnas.0903186107

Fig. 2.

Fig. 2.

(A) As in Fig. 1B but for the selected models from the WCRP CMIP3 multimodel dataset. Here the fractional changes of climatological-mean precipitable water (shown within the parentheses in the legends) have been subtracted from each model’s fractional changes of precipitation. (B) As in (A) but for 30–60°N.