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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 8, issue 24
Atmos. Chem. Phys., 8, 7389-7403, 2008
https://doi.org/10.5194/acp-8-7389-2008
© Author(s) 2008. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 8, 7389-7403, 2008
https://doi.org/10.5194/acp-8-7389-2008
© Author(s) 2008. This work is distributed under
the Creative Commons Attribution 3.0 License.

  12 Dec 2008

12 Dec 2008

Model analysis of the factors regulating the trends and variability of carbon monoxide between 1988 and 1997

B. N. Duncan1,2 and J. A. Logan3 B. N. Duncan and J. A. Logan
  • 1Goddard Earth Sciences and Technology Center, University of Maryland at Baltimore County, Baltimore, MD, USA
  • 2NASA Goddard Space Flight Center, Code 613.3, Greenbelt, MD, USA
  • 3School of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USA

Abstract. We used a 3-D model of chemistry and transport to investigate trends and variability in tropospheric carbon monoxide (CO) for 1988–1997 caused by changes in the overhead ozone column, fossil fuel emissions, biomass burning emissions, methane, and transport. We found that the decreasing CO burden in the northern extra-tropics (−0.85%/y) was more heavily influenced by the decrease in European emissions during our study period than by the similar increase in Asian emissions, as transport pathways from Europe favored accumulation at higher latitudes in winter and spring. However, the opposite trends in the CO burdens from these two source regions counterbalanced at lower latitudes. Elsewhere, the factors influencing CO often compete, diminishing their cumulative impact, and trends in model CO were small or insignificant for our study period, except in the tropics in boreal fall (1.1%/y), a result of emissions from major fires in Indonesia late in 1997. There was a decrease in the ozone column during the study period as a result of the phase of the solar cycle and the eruption of Pinatubo in 1991. This decrease contributed negatively to the trend in model CO by increasing the hydroxyl radical (OH). The impact of this negative contribution was diminished by a positive contribution of similar magnitude from increasing methane. However, the trends in these two factors did not cancel for tropospheric OH, which responded primarily to changes in the ozone column.

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