Fig. 8From: Toward reduction of the uncertainties in climate sensitivity due to cloud processes using a global non-hydrostatic atmospheric modelLongwave cloud feedback [W m−2 K−1] on International Satellite Cloud Climatology Project (ISCCP) diagrams estimated from the cloud radiative kernel. Longwave cloud feedback in a NSW6-JJA and b NDW6-JJA are plotted in the ISCCP diagram with cloud top pressure (vertical axis) and cloud optical depth (lateral axis). Adapted from Chen et al. (2016)Back to article page