Volcanoes emit a significant amount of microscopic gas and
ash particles into the atmosphere when they erupt, which become atmospheric aerosols. By increasing the number of aerosol particles through gas-to-particle conversion processes, the contents of these eruptions can then affect the concentrations of potential cloud condensation nuclei (CCN) and
ice nucleating particles (INP), which in turn affects cloud properties and leads to changes in local or regional climate. Of these gases, sulfur dioxide, carbon dioxide, and water vapour are most commonly found in volcanic eruptions. While water vapour and carbon dioxide CCNs are naturally abundant in the atmosphere, the increase of sulfur dioxide CCNs can impact the climate by causing
global cooling. Almost 9.2 Tg of sulfur dioxide () is emitted from volcanoes annually. This sulphur dioxide undergoes a transformation into
sulfuric acid, which quickly condenses in the stratosphere to produce fine sulphate aerosols. The Earth's lower atmosphere, or troposphere, cools as a result of the aerosols' increased capability to reflect solar radiation back into space. ==Effect on air pollution==