Fig. 9From: Toward reduction of the uncertainties in climate sensitivity due to cloud processes using a global non-hydrostatic atmospheric modelThe zonal mean distribution of cloud changes. Cirrus cloud changes (red lines) and longwave cloud feedback contributed by cirrus clouds changes (blue lines) are shown for a NSW6-JJA and b NDW6-JJA. Note that the longwave cloud radiative feedback are calculated using the cloud radiative kernel proposed by Zelinka et al. (2012). Adapted from Chen et al. (2016)Back to article page