Fig. 3
From: Extreme wet and dry conditions affected differently by greenhouse gases and aerosols
Relative changes in the frequency of different precipitation amounts for individual models and forcing agents. Note that here, the changes are not normalized by the magnitude of the global temperature change ΔT, which instead is provided in the barplot insets in each figure panel. Gray lines show “background” variation (based on the years 1–100 of the BASE simulations) calculated from Monte Carlo simulations, as an indication of natural variability
