Aerosols are any small liquid or solid particles suspended in the atmosphere, excluding large cloud or precipitation particles. They are released into the atmosphere by both natural and anthropogenic sources, and interact with various global systems in complex ways.
Two major interactions of aerosols with the environment are radiative forcing (how the particles interact with incoming sunlight), and cloud interactions. These interactions impact the global climate in many ways which will be explored on this page.
Aerosols vary greatly in size, composition and shape, and their lifespan depends on their location in the atmosphere, lasting anywhere from a couple of weeks up to a year. Examples of natural aerosols include dust, such as from deserts, and volcanic aerosols such as volcanic sulfur oxides. Anthropogenic aerosols include particulate matter (PM) such as soot and coal ash, forms of dust, smoke, and more.
Overall, models and observational evidence show that aerosols as a whole exert a cooling effect on the planet - in effect masking some of the global warming from greenhouse gases that would otherwise occur in their absence. There is, however, a projected decrease in the anthropogenic emissions of aerosols due to new air quality policies, which would eventually unmask this warming.
These two interactions have a modifying effect on Earth's heat balance. The balance between these interactions depends on the specific particles and environmental conditions in a given region, and determining their global impact requires satellite data and computer models. Most studies agree that the overall effect from these interactions is to cool the Earth.
Aerosols serve as a site for cloud droplets and ice particles to form. When there are more aerosols present, clouds tend to have a large amount of tiny particles, which causes these clouds to reflect more solar radiation. Although modelling and analyzing these systems is difficult, available studies generally indicate that through cloud interactions aerosols increase the overall cooling effect present from their radiation interactions.