Chapter 3 Aerosol-Climate Interactions

摘要: Publisher Summary This chapter discusses the aerosol–climate interactions and is devoted to direct radiative effects of aerosols. Aerosol layers are composed submicrometer-sized particles that can be treated independently larger in clouds a budget Earth's atmosphere. The place forcing by tropospheric aerosols overall scheme presented. Any estimates only translated into climate response accepting verisimilitude current models. relationship between feedbacks determines role play maintenance radiation balance. Occasionally, natural or anthropogenic events create locally severe aerosol loads could lead large climatic perturbations. One example springtime Arctic haze has been studied for several years. Most atmospheric origin sulfates smoke, which have residence times troposphere about week; contrast greenhouse gases lifetimes decades centuries. A reduction emission sulfur-containing gases, primary precursors sulfate aerosols, would result an immediate concomitant decrease negative shortwave system.