Chemistry of Atmospheric Aerosols
In recent years, the role of atmospheric aerosols is being increasingly recognized both in climate system of Earth and in global biogeochemical cycle. Aerosols affect the radiative balance of the Earth directly by scattering or absorbing incoming shortwave radiation and indirectly by acting as cloud condensation nuclei, altering a temperature effect at the surface because of changes in cloud cover. In addition, aerosol particles are closely coupled to atmospheric chemistry as chemical reactions in the atmosphere are often accelerated on aerosol surfaces. Also, the chemistry of aerosols may alter their physical and optical properties such as size distribution (fine to coarse) due to interaction between acidic (sulpahte, nitrate) and alkaline (mineral dust) aerosols; single scattering albedo (because of coating of one type of aerosols over other); and surface properties (hydrophilic/hydrophobic), and thus, their direct and indirect effects on climate change. Long range transport and depo...