Pre-industrial dust rise and 1980s peak (1850s–1980s)
Dust mass loading increased roughly 55 ± 30 percent since pre-industrial times, driven largely by rising emissions from Asia and North Africa as agriculture, grazing, and water diversions expanded arid land.
By the 1980s, atmospheric dust reached its modern maximum, exerting a net cooling effect of about −0.07 ± 0.18 W/m² that partially offset greenhouse warming.
The increase set a baseline that made the recent decline measurable and gave scientists a reference point for today's still-elevated dust levels.
Today's dust decline reverses a century-long increase, which is why its warming effect matters — it partly unwinds a natural cooling buffer that had been growing.
