Fig. 10From: Recent global nonhydrostatic modeling approach without using a cumulus parameterization to understand the mechanisms underlying cloud changes due to global warmingComposite of future minus past precipitation amount averaged over all the oceanic extratropical cyclones (top row) and the intense oceanic extratropical cyclones (bottom row) for (left to right): 56Â km, 28Â km, and 14Â km mesh models. Gray circles indicate the distance from the center of the extratropical cyclone in intervals of 500Â kmBack to article page