Fig. 1: The spatio-temporal distributions of the Aerosol Direct Radiative Effect (ADRE) and aerosol short-wave radiative warming effect (AWE).
From: Surface albedo regulates aerosol direct climate effect
(a) the spatial distribution of the multi-year average ADRE from March 2000 – February 2020; (b) similar to (a), but for the AWE; (c) similar to (b), but depicting the frequency of AWE; (d) the spatial distribution of multi-year average AWE and occurrence frequency at AERONET sites, where the size of the circles represents the frequency of AWE at each site, and the color indicates the average value of AWE. Note that both the ADRE and AWE are in the clear-sky condition.
