The sampling site on Amsterdam Island is operated in cooperation with the French Centre des Faibles Radioactivités. Except during the summer (December?February), when this island is within the wind regime of the westerlies, the monthly mean mixing ratios from Amsterdam Island can be considered representative of the background subantarctic atmosphere (Gaudry et al. 1983).
The NOAA flask data from Amsterdam Island show an increase in the
annual value from 341.1 parts per million (ppm) in 1983 to
350.5 ppm in 1989 or 1.6 ppm per year. Conway et al. (1994)
reported a global growth rate of 1.43 ppm per year for
1981-92 for all NOAA/CMDL flask-sampling sites.
Ascencio-Parvy et al. (1983) found a 0.11 ppm-per-month increase in
atmospheric CO concentrations at Amsterdam Island from
October 1980 to November 1983. Both Conway et al. (1988) and
Ascencio-Parvy et al. (1984) found considerable variability within
each year and suggested that the growth rate minimum in 1982 and
the growth rate maximum in 1983 may result partly from the 1982-83
El Niño event.

Date revised 4/10/95 (gg)
records from sites in the NOAA/CMDL air
sampling network. In
T.A. Boden, D.P. Kaiser, R.J. Sepanski, and F.W. Stoss (eds.),
Trends '93: A Compendium of Data on Global Change. ORNL/CDIAC-65.
Carbon Dioxide Information Analysis Center, Oak Ridge National
Laboratory, U.S. Department of Energy, Oak Ridge, Tenn., U.S.A.
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