Evidence from the Pacific troposphere for large global sources of oxygenated organic compounds

H. Singh (), Y. Chen, A. Staudt, D. Jacob, D. Blake, B. Heikes and J. Snow
Additional contact information
H. Singh: NASA Ames Research Center
Y. Chen: NASA Ames Research Center
A. Staudt: Harvard University
D. Jacob: Harvard University
D. Blake: University of California
B. Heikes: University of Rhode Island
J. Snow: University of Rhode Island

Nature, 2001, vol. 410, issue 6832, 1078-1081

Abstract: Abstract The presence of oxygenated organic compounds in the troposphere strongly influences key atmospheric processes. Such oxygenated species are, for example, carriers of reactive nitrogen and are easily photolysed, producing free radicals1,2,3—and so influence the oxidizing capacity and the ozone-forming potential of the atmosphere4,5,6—and may also contribute significantly to the organic component of aerosols7,8. But knowledge of the distribution and sources of oxygenated organic compounds, especially in the Southern Hemisphere, is limited. Here we characterize the tropospheric composition of oxygenated organic species, using data from a recent airborne survey9 conducted over the tropical Pacific Ocean (30° N to 30° S). Measurements of a dozen oxygenated chemicals (carbonyls, alcohols, organic nitrates, organic pernitrates and peroxides), along with several C2–C8 hydrocarbons, reveal that abundances of oxygenated species are extremely high, and collectively, oxygenated species are nearly five times more abundant than non-methane hydrocarbons in the Southern Hemisphere. Current atmospheric models are unable to correctly simulate these findings, suggesting that large, diffuse, and hitherto-unknown sources of oxygenated organic compounds must therefore exist. Although the origin of these sources is still unclear, we suggest that oxygenated species could be formed via the oxidation of hydrocarbons in the atmosphere, the photochemical degradation of organic matter in the oceans, and direct emissions from terrestrial vegetation.

Date: 2001
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DOI: 10.1038/35074067

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