作者: S. Madronich , C. Granier
DOI: 10.1007/978-3-642-78884-0_1
关键词:
摘要: UV radiation is a principal driving force of tropospheric chemistry. Increases in UV, calculated to result from stratospheric O3 depletion, are likely increase the reactivity troposphere, and thus change concentrations key species such as OH, CH4, O3, H2O2. The geographical distributions other species, SO2 NOx, also be altered. Further study needed for quantitative assessment these indirect chemical effects depletion.