Causes: Cooling effect of aerosol emissions
Image: Peggy Anke
-
Fig. 1: The climate forcings that have contributed to climate change from 1850 to 2023.The black line shows the observed global surface temperatures since 1850. ‘Natural’ forcings (green line) include volcanic eruptions (such as Mt. Pinatubo in 1991) which together generally cooled the atmosphere for short periods. It’s clear that the cooling effect of volcanic eruptions and even greater cooling effect of aerosol emissions during this period offset some of the warming. When added together, however (amber line), all of the cooling forcings aren’t enough to offset the main warming forcing: greenhouse gases (grey line) (Image: Zeke Hausfather, January 2025).




