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U.S. Department of Energy
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The role of atmospheric chemistry in climate change

Conference ·
OSTI ID:7166168

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 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, we examine the importance of chemical processes and other interactions in determining climatic change and future policy options. 28 refs., 3 figs., 2 tabs.

Research Organization:
Lawrence Livermore National Lab., CA (USA)
DOE Contract Number:
W-7405-ENG-48
OSTI ID:
7166168
Report Number(s):
UCRL-97811; CONF-880679-8; ON: DE88012439
Country of Publication:
United States
Language:
English