Atmospheric lifetime experiment. 5. Results for CH/sub 3/CCl/sub 3/ based on three years of data

Journal Article · Thu Oct 20 04:00:00 EDT 1983 · J. Geophys. Res.; (United States)

DOI:https://doi.org/10.1029/JC088iC13p08415· OSTI ID:6750731

Prinn, R G; Rasmussen, R A; Crawford, A J; Simmonds, P G; Alyea, F N; Cunnold, D M; Lane, B C

We present gas chromatographic determination of the concentrations of CH/sub 3/CCl/sub 3/ at Adrigole (Ireland), Cape Meares (Oregon), Ragged Point (Barbados), Point Matatula (American Samoa), and Cape Grim (Tasmania) for the 3-year period July 1978 through June 1981. The determinations involve approximately four measurements each day with on-site calibration. The absolute values and trends for these observed concentrations are interpreted in terms of the industrial production, global circulation rate, and atmospheric lifetime of CH/sub 3/CCl/sub 3/ by using an optimal estimation technique that incorporates a nine-box model of the atmosphere. The globally and annually averaged trend in the lower troposphere at the midpoint of the second year of the experiment is 8.7% per year, and the inferred global atmospheric content of CH/sub 3/CCl/sub 3/ at this midpoint is 2.58 x 10/sup 9/kg. The global atmospheric lifetime deduced by using the observed trends and global content together with current estimates of industrial CH/sub 2/CCl/sub 3/ emissions at 10.2/sup +5.2//sub -2.6/ years. This deduced lifetime is sufficiently going to imply that the observed variability in the data on seasonal and shorter time scales must be dominated by meteorological (and perhaps industrial emission) variabilities rather than by spatial and temporal variations in the rate of chemical destruction of CH/sub 3/CCl/sub 3/ by OH. However, the observed variations on annual and longer time scales are sensitive to the spatially and temporally averaged OH concentrations. In particular, the globally averaged tropospheric OH concentration compatible with the above-deduced CH/sub 3/CCl/sub 3/ lifetime is (5 +- 2) x 10/sup 5/ molecule cm/sup -3/; in reasonable agreement, for example, with the value of (6.5/sup +3//sub -/2) x 10/sup 5/ molecule cm/sup -3/ deduced by Volz et al. (1981) from measurements of CO.

• Research Organization: Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology
• OSTI ID: 6750731
• Journal Information: J. Geophys. Res.; (United States), Journal Name: J. Geophys. Res.; (United States) Vol. 88:C13; ISSN JGREA
• Country of Publication: United States
• Language: English

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