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AGU: Geophysical Research Letters

 

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A large terrestrial source of methyl iodide

It has been known that methyl iodide (CH3I), a compound that influences ozone chemistry and aerosol formation in the atmosphere, is released primarily from the ocean. Sive et al. (2007) recently identified terrestrial sources of CH3I using a synthesis of field observations, including research flights over the United States and the North Atlantic, a ground-based atmospheric observation network in New England, and a field campaign at Duke Forest, North Carolina. The authors found that about 2700 ng of CH3I per square meter are released each day from midlatitude vegetation and soils, a value similar in magnitude to previous estimates of the oceanic source strength. They expect that similar studies to measure CH3I emitted from tropical and boreal areas will improve flux estimates and facilitate the development of a more accurate global budget for CH3I.

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Published: 06 September 2007

Citation: Sive, B. C., R. K. Varner, H. Mao, D. R. Blake, O. W. Wingenter, and R. Talbot (2007), A large terrestrial source of methyl iodide, Geophys. Res. Lett., 34, L17808, doi:10.1029/2007GL030528.