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U.S. Department of Energy
Office of Scientific and Technical Information

The role of atmospheric chemistry in climate change

Conference ·
OSTI ID:6943298
Surface emissions and concentrations of globally important trace gases are increasing. Climate models indicate significant temperature increases could occur in the next century due to increasing CO{sub 2} concentrations. However, the combined direct radiative effects from other trace gases could be as large as those estimated for CO{sub 2}. Many of these gases also have indirect effects on climate through their chemical interactions with other radiatively important atmospheric constituents. For example, within the troposphere, emissions of CH{sub 4}, CO, and NO{sub x} may increase concentrations of ozone, an important radiatively active gas. These emissions may also effect concentrations of hydroxyl (OH), which, while not radiatively important, has an important impact on tropospheric chemistry and on the concentrations of long-lived gases reaching the stratosphere. In the stratosphere, dissociation of CH{sub 4}, N{sub 2}O, and the CFCs can lead to changes in the ozone distribution. Oxidation of increasing CH{sub 4} concentrations would increase stratospheric concentrations of radiatively important water vapor. Climate change can, on the other hand, alter tropospheric H{sub 2}O concentrations, further affecting chemistry impacts on climate. In this paper.
OSTI ID:
6943298
Report Number(s):
CONF-880679--
Country of Publication:
United States
Language:
English