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Atmospheric Trends of Carbon Monoxide (CO) by Khalil and Rasmussen
Entry ID:
OGI_CO_TRENDS
Summary
Abstract:
Carbon monoxide (CO) is a weak greenhouse gas but it is an important
precursor to tropospheric ozone (O3) and other trace gases in the Earth's atmosphere, which can cause widespread changes in tropospheric chemistry, global warming, and other climatic changes. Hydroxyl (OH) radicals in the global atmosphere are removed primarily through reactions with CO. OH radicals ... ![]() Geographic Coverage
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Temporal Coverage
Start Date:
1979-07-01
Stop Date:
1987-12-31
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Publications/References
Khalil, M.A.K., and R.A. Rasmussen. 1984. 'Carbon monoxide in the Earth's
atmosphere: Increasing Trend', Science, Vol. 224, pp. 54-56. Khalil, M.A.K., and R.A. Rasmussen. 1988. 'Carbon monoxide in the Earth's atmosphere: Indications of a global increase', Nature, Vol. 332, pp. 242-245. Logan, J.A., M.J. Prather, S.C. Wofsy, and M.B. McElroy. 1981. 'Tropospheric chemistry: A global perspective', J. Geophys. Res., Vol. 86 (C8), pp. 7210-7254. Creation and Review Dates
Last DIF Revision Date:
2010-07-07
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