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Atmospheric Carbon Dioxide Record from Mauna Loa, Hawaii, USAInvestigatorsL.P. Steele, P.B. Krummel and R.L. Langenfelds
Period of RecordJune 1991 - December 2006 MethodsIndividual measurements have been obtained from flask air samples returned to the CSIRO GASLAB. Typical sample storage times range from days to weeks for some sites (e.g. Cape Grim, Aircraft over Tasmania and Bass Strait) to as much as one year for Macquarie Island and the Antarctic sites. Experiments carried out to test for changes in sample CO2 mixing ratio during storage have shown significant drifts in some flask types over test periods of several months to years (Cooper et al., 1999). Corrections derived from the test results are applied to network data according to flask type. Samples were analysed by gas chromatography with flame ionization detection after methanization of CO2 to CH4. One Carle gas chromatograph, labeled "Carle-3" (C3) was used over the length of the record. Further details of CSIRO's global sampling network, sampling procedure, and analytical techniques are provided elsewhere (e.g., Francey et al., 1996); measurement uncertainty is discussed by Langenfelds et al. (2001). Data are reported in the WMO CO2 Mole Fraction Scale. The link to this scale was established with nine 'primary' high-pressure cylinder standards of synthetic mixtures of CO2 and CO in "zero air" (hydrocarbon-free air) calibrated by NOAA/CMDL in 1992, with a subset recalibrated in 1994. The relative stability of the primary suite is monitored using frequent comparisons with about 15 long-lived secondary standards. The link to the international scale is monitored by a variety of on-going comparisons involving high-pressure cylinder standards (e.g., WMO Round Robins, IAEA CLASSIC, cylinder exchanges with NOAA, etc.), as well as 6-per-month flask-air-sharing comparisons of samples collected at Cape Grim. More detailed calibration information is given by Langenfelds 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).
Manua Loa, Hawaii, USA
TrendsThese measurements indicate a rise in annual average atmospheric CO2 concentration from 356.65 parts per million by volume (ppmv) in 1992 to 381.74 ppmv in 2006, or an increase of about 1.79 ppmv/year, on average. These data may be compared with flask samples taken by the National Oceanic and Atmospheric Administration (NOAA), Geophysical Monitoring Division (GMD), which show an increase from 356.58 ppmv in 1992 to 381.88 ppmv in 2006, or an average increase of about 1.81 ppmv/year. Another possible comparison is with continuous measurements made through 2004 by the Scripps Institution of Oceanography; these data are also available in TRENDS. The Scripps data show an increase from 356.37 ppmv in 1992 to 377.38 ppmv in 2004, or an increase of 1.75 ppmv/year. The corresponding (1992-2004)average change for these CSIRO flask data is 1.73 ppmv/year. Differences are partly due to different sampling methods; the CSIRO (flask) data are taken at particular times, while the Scripps and NOAA/CMDL data represent continuous measurements. There are also differences in statistical treatment of the data (e.g., acceptance criteria, smoothing techniques), as well as instrument differences which are discussed by Masarie et al. (2001). References
CITE AS: Steele, L. P., P. B. Krummel and R. L. Langenfelds. 2007. Atmospheric CO2 concentrations from sites in the CSIRO Atmospheric Research GASLAB air sampling network (August 2007 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. December 2007 |