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Subject Areas
Carbon Cycle
Climate
Coastal Sensitivity to Sea Level Rise
Energy and Socioeconomic Systems
Land-Use and Ecosystems
Oceanic Trace Gases
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Vegetation Response to CO2 and Climate
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Atmospheric Trace Gas Measurements
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Atmospheric Methane Record from Mawson, AntarcticaInvestigatorsL.P. Steele, P.B. Krummel and R.L. Langenfelds
Period of RecordMay 1984 - December 2001 MethodsThe listed data have been obtained from flask air samples returned to the CSIRO GASLAB for analysis. Typical sample storage times range from days to weeks for some sites (e.g., Cape Grim) to as much as one year for Macquarie Island and the Antarctic sites. Experiments carried out to test for any change in sample CH4 mixing ratio during storage have shown no drift to within detection limits over test periods of several months to years (Cooper et al., 1999). Samples were analysed by gas chromatography with flame ionization detection (FID). Three individual but similarly configured Carle gas chromatographs were used over the length of the record. They are labeled "Carle-1" (C1), "Carle-2" (C2) and "Carle-3" (C3). Further details of CSIRO's global sampling network, sampling and analytical techniques are provided by Francey et al. (1996); measurement uncertainty is discussed by Langenfelds et al. (2001). Data are reported in the CSIRO94 CH4 scale (Steele et al., 1996), which is derived from the CH4 scale maintained at NOAA/CMDL (Dlugokencky et al., 1994). The link to this scale was established with two high pressure cylinders containing dry, natural air that were calibrated by NOAA/CMDL between 1987 and 1990. Results from later exchanges of high-pressure cylinders indicate a small, but measurable difference (0.36 ±0.17 ppbv). Stability of the CSIRO scale is monitored with approximately 25 assorted long-lived standards. More detailed calibration information is given by Langenfelds et al. (2001). Comparison of CSIRO and NOAA flask measurements indicates agreement to within 1 ppbv (Masarie et al., 2001). These data represent monthly means, calculated as the mean of daily values from a smooth curve fit to the data using the curve-fitting routines described by Thoning et al. (1989).
Mawson, Australia
TrendsA clear annual cycle in methane concentration is evident, largely due to increase in its destruction by the OH radical during the summer months. Air arriving at Mawson is well mixed, having recently traveled over the Southern Ocean, and is far removed from spatial and seasonal variations in source strength characteristic of land areas. An average increase of around 12 ppbv/year from 1985 through 1991 was followed by a reduced rate of increase, averaging 5 ppbv/year, until 1999. Since 1999, the increase has been very slight; and a decrease occurred from 2000 to 2001. This pattern is remarkably similar to that for Cape Grim, Australia. References
CITE AS: Steele, L. P., P. B. Krummel and R. L. Langenfelds. 2002. Atmospheric CH4 concentrations from sites in the CSIRO Atmospheric Research GASLAB air sampling network (October 2002 version). In Trends: A Compendium of Data on Global Change, Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, U.S. Department of Energy, Oak Ridge, TN, U.S.A. January 2003 |
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