Extended Data Fig. 8: Difference in stratiform low cloud fraction (LCF) at 925 hPa in northern-hemisphere summer.
From: Substantial influence of vapour buoyancy on tropospheric air temperature and subtropical cloud
Each panel is calculated as the difference between the average LCF of Group A models and LCF of individual Group B models. All panels correspond to the same model in Extended Data Fig. 6. Positive values mean that Group B models have lower LCF.
