• 2025-11-07

Aerosol

Aerosol

An aerosol is a system of solid or liquid particles dispersed in the atmosphere, with particle sizes typically ranging from 0.01 to 10 μm. Its natural sources include:

Marine sources: Sea salt particles (NaCl, MgSO₄) generated by the evaporation of wave spray

Terrestrial sources: Silicate mineral particles carried by wind-blown dust

Biogenic source: Oxidation products of plant volatile organic compounds

Climate regulation mechanism

■ Radiative forcing effect

Cooling effect:

Sulfate/nitrate aerosols reflect solar shortwave radiation (albedo increases by 0.01-0.1)

For every 1 W/m² increase in aerosol radiative forcing, surface temperature decreases by 0.5±0.2℃

Warming effect:

Black carbon and other light-absorbing aerosols absorb longwave radiation (absorption efficiency > 0.8)

■ Cloud physical effects

As cloud condensation nuclei (CCN), they change the cloud droplet size distribution, extend cloud lifespan, and enhance albedo