Abstract

Abstract. We analyze the North American budget for carbon monoxide using data for CO and formaldehyde concentrations from tall towers and aircraft in a model-data assimilation framework. The Stochastic Time-Inverted Lagrangian Transport model for CO (STILT-CO) determines local to regional-scale CO contributions associated with production from fossil fuel combustion, biomass burning, and oxidation of volatile organic compounds (VOCs) using an ensemble of Lagrangian particles driven by high resolution assimilated meteorology. In many cases, the model demonstrates high fidelity simulations of hourly surface data from tall towers and point measurements from aircraft, with somewhat less satisfactory performance in coastal regions and when CO from large biomass fires in Alaska and the Yukon Territory influence the continental US. Inversions of STILT-CO simulations for CO and formaldehyde show that current inventories of CO emissions from fossil fuel combustion are significantly too high, by almost a factor of three in summer and a factor two in early spring, consistent with recent analyses of data from the INTEX-A aircraft program. Formaldehyde data help to show that sources of CO from oxidation of CH4 and other VOCs represent the dominant sources of CO over North America in summer.

Highlights

  • Carbon monoxide is a key species for both atmospheric chemistry and public health

  • The results show that volatile organic compounds (VOCs) and CH4 sources of CO significantly exceed anthropogenic CO emissions during summer months, even in areas of relatively lower biogenic VOC emissions such as in Wisconsin and the upper Midwest

  • Stochastic Time Inverted Lagrangian Transport Model (STILT)-CO produces hourly results for carbon monoxide concentrations that closely correlate with measurements at a tall tower site and from aircraft

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Summary

Introduction

Carbon monoxide is a key species for both atmospheric chemistry and public health. In the United States, it is one of the original six criteria air pollutants in the Clean Air Act of 1970, and many urban areas remain either in violation of ambient CO air quality standards or at risk of violation (US EPA, 2007b). Carbon monoxide plays important roles in ozone production, in regulating concentrations of OH radicals, and indirectly in climate forcing (Thompson, 1992; Daniel and Solomon, 1998; Warneke et al, 2006). Motor vehicle exhaust accounts for 85–95% of fossil fuel sources (US EPA, 2007a). The principal sink for CO is oxidation by the OH radical, giving a mean atmospheric lifetime of two months (Logan et al, 1981)

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