Extended Data Fig. 2: Spatially-resolved SLH-driven radiative effect of the main short-lived climate forcers during future scenarios.
From: Natural short-lived halogens exert an indirect cooling effect on climate

The individual RE contribution arising from methane (a,b), ozone (c,d) and aerosols (e,f) at the top of the model are shown for the AANE+ANT configuration in year 2100 for the RCP 6.0 (left column) and RCP 8.5 (right column) scenarios. Equivalent panels for pre-industrial and present-day conditions are shown in Fig. 2. All maps and elements were created by our research group using Matplotlib Basemap for Phyton.