作者: T. Hoffmann
DOI: 10.1007/978-3-642-56722-3_23
关键词:
摘要: Atmospheric aerosols scatter sunlight, serve as condensation nuclei for cloud droplet formation and participate in heterogeneous chemical reactions. Hence, they play an important role global climate atmospheric chemistry. As a result of numerous field studies carried out the last few years, it became obvious that, frequently, organic matter dominates composition submicrometer aerosols, especially over continental regions (Novakov et al., 1997; Murphy Thomson, 1997).