Atmospheric Aerosol Loading is measured by aerosol optical depth (AOD). AOD is an integrated measure of the overall reduction in sunlight reaching Earth’s surface caused by all absorption and scattering in the vertical air column. Richardson et al.2023

Studies suggest that a raised interhemispheric AOD difference caused by persistent and widely distributed aerosol emissions could lead to major reductions in precipitation in the tropics. Richardson et al.2023


⁞⁞ Earth-system process ⁞⁞ Regenerative strategies ⁞⁞


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