Abstract. Atmospheric aerosol particles are known to contain organic carbon material in variable amounts, depending on their location. In some parts of the world, organic compounds make up the majority of the total suspended particle mass. This class of particulate matter is important in a wide range of geophysical and environmental problems, ranging from local issues (e.g., pollution toxicity) to the global scale (e.g., climate change). Unfortunately, the richness of organic chemistry and the highly variable physical properties associated with both natural and anthropogenic organic particles lead to great difficulties in sampling and obtaining complete chemical information on these materials. These obstacles result in an incomplete picture of a potentially significant part of atmospheric chemistry and a correspondingly poor understanding of the geophysical and environmental effects of this aerosol. Given the paucity of quantitative molecular data, the purpose of this paper is not to quantitatively describe the importance of organic aerosols in environmental issues, but rather to present a basis for defining what data are needed. With this goal in mind, we begin with an overview of the major environmental issues known to be affected by organic aerosols, followed by a description of the distribution, sources, and chemical and physical properties of organic aerosols as they are currently understood. Methods used to collect and study organic aerosols are provided, followed by a list of outstanding scientific questions and suggestions for future research priorities. mental Protection Agency (U.S. EPA), 1996]. This fraction has been studied extensively, and several models of the geographical distribution and climatic effects of this group of compounds in the aerosol have appeared [IPCC, 1995]. While somewhat less studied, the insoluble inorganic fraction has been analyzed, for example, with nuclear methods, and generally consists of metal oxides, silicates, and clay minerals derived from soil dust. Unlike the salt and soil dust fractions, the organic compounds cover a very wide range of molecular forms, solubilities, reactivities, and physical properties, which makes a complete characterization extremely difficult. The so-called "elemental" carbon (EC) aerosol has been studied extensively, but it is still not clear to what degree it is indeed elemental [graphitic, C(0)] material or high molecular weight refractory organic species or a combination of both. Consequently, there is still no complete inventory of the chemical compounds that compose the fine-particle organic aerosol from any site in the world, and there is only a limited understanding of the sources, sinks, transport, and transformation processes of these particles and their effects. Since organic compounds are usually the second most abundant component of fine aerosol after sulfates [Heintzenberg, 1989; White, 1990; U.S. EPA, 1996], our understanding of the numerous