Science in China Series D: Earth Sciences

, Volume 52, Issue 11, pp 1857–1863 | Cite as

The characteristics of atmospheric CO2 concentration variation of four national background stations in China

  • LiXin Liu
  • LingXi Zhou
  • XiaoChun Zhang
  • Min Wen
  • Fang Zhang
  • Bo Yao
  • ShuangXi Fang
Article

Abstract

Atmospheric carbon dioxide is an important kind of greenhouse gas which influences global temperature. Its concentration variation could indicate the distribution of human and natural activities in various regions. Through the non-dispersive infrared method, flask sampling of atmospheric CO2 concentration was measured weekly at four national background stations including Waliguan, Shangdianzi, Lin’an, and Longfengshan. Based on the data collected from September 2006 to August 2007, along with the Waliguan station’s experience on in situ observational data processing, the selection methods for sampling data through the atmospheric background CO2 concentration analysis were preliminarily discussed. On the basis of this result, the variation features of the four typical regions’ atmospheric background CO2 concentration was analyzed for the first time. The results show that the atmospheric CO2 concentration at Waliguan, Shangdianzi, Lin’an, and Longfengshan is 383.5, 385.9, 387.8, and 384.3 ppm, respectively. During the research period, CO2 concentration at the Waliguan station changed slightly. However, the CO2 concentration changed sharply at the Shangdianzi and the Lin’an stations due to the great influence of human activities in the Jingjinji and the Changjiang Delta economic zones, and changed regularly with seasons at Longfengshan station under dual influences of human activities and plant photosynthesis. The results from this study can lay the foundation for more profound studies on atmospheric CO2 concentration level of different areas in China, and could be used to improve the understanding of carbon source and sink distribution.

Keywords

atmospheric CO2 flask sampling background data selection CO2 concentration regional difference 

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References

  1. 1.
    Intergovernmental Panel on Chimate Change (IPCC). Climate Change 2007: The Physical Science Basis. Cambridge: Cambridge University Press, 2007Google Scholar
  2. 2.
    World Meteorological Organization (WMO). Greenhouse Gas Bulletin: The State of Greenhouse Gases in the Atmosphere Using Global Observations through 2006. 2007Google Scholar
  3. 3.
    Komhyr W D, Gammon R H, Harris T B, et al. Global atmospheric CO2 distribution and variations from 1968–1982 NOAA/GMCC CO2 flask sample data. J Geophys Res, 1985, 90: 5567–5596CrossRefGoogle Scholar
  4. 4.
    Keeling C D. Atmospheric carbon dioxide variations at Mauna Loa observatory, Hawaii. Tellus, 1976, 28: 538–551CrossRefGoogle Scholar
  5. 5.
    Conway T J, Tans P P, Waterman L S, et al. Evidence for inter-annual variability of the carbon cycle from the NOAA/CMDL global air sampling network. J Geophys Res, 1994, 99: 22831–22855CrossRefGoogle Scholar
  6. 6.
    Alison C E. δ 13C of atmospheric CO2 at Cape Grim: The in situ record, the flask record, air standards and the CG92 calibration scale. In: Dick A L, Bouma W, Derek N, eds. Baseline Atmospheric Program (Australia) 1996. Victoria: Bureau of Meteorology and CSIRO Division of Atmospheric Research, Melbourne, 1999. 45–56Google Scholar
  7. 7.
    WMO. 12th WMO/IAEA Meeting of Experts on Carbon Dioxide Concentration and Related Tracers Measurement Techniques. No. 161. Toronto, Canada, 2005Google Scholar
  8. 8.
    Wen Y P, Tang J, Shao Z Q, et al. A study of atmospheric CO2 concentration variations and emission from the soil surface at Mt. Waliguan (in Chinese). Q J Appli Meteorol, 1997, 8(2): 129–136Google Scholar
  9. 9.
    Wang M L, Li X S. Analysis on the concentration of CH4, CO2 and CO in atmosphere watch observatory. In: Li Q S, ed. Analysis on Atmospheric Trace Gas and Other Chemical Substance in China and West Pacific (in Chinese). Beijing: China Meteorological Press, 1986. 172–185Google Scholar
  10. 10.
    Wang M X, Liu W W, Rasmussen R A, et al. The long seasonal change trends of Atmosphere CH4 in the desert area of Northwest China. Chin Sci Bull, 1989, 9: 684–686Google Scholar
  11. 11.
    Wang G C, Wen Y P, Kong Q X, et al. The concentration of CO2 and its variation in China. Chin Sci Bull, 2002, 47(10): 780–783Google Scholar
  12. 12.
    Wang C K, Wang Y S, Liu G R. Characteristics of atmospheric CO2 variations and some affecting factors in urban area of Beijing (in Chinese). Environ Sci, 2003, 24(4): 13–17Google Scholar
  13. 13.
    Zhou X J. The Summary Report of China Atmosphere Watch Baseline Observatory. Beijing: China Meteorological Press, 2005Google Scholar
  14. 14.
    Zhou L X, Thomas J C, James W C, et al. Long-term record of atmospheric CO2 and stable isotopic ratios at Waliguan Observatory: Background features and possible drivers, 1991–2002. Global Biogeochem Cycles, 2005, 19: GB3021, doi: 10.1029/2004GB002430CrossRefGoogle Scholar
  15. 15.
    Zhou L X, Zhou X J, Zhang X C, et al. Progress in the study of background greenhouse gases at Waliguan observatory. Acta Meteorol Sin, 2007, 65(3): 458–468Google Scholar
  16. 16.
    Tans P P, Thoning K W, Elliott W P, et al. Background Atmospheric CO2 Patterns from Weekly Flask Samples at Barrow, Alaska: Optimal Signal Recovery and Error Estimates, in NOAA Tech. Memo (ERL ARL-173). Environmental Research Laboratories, Boulder, CO, 1989. 131Google Scholar
  17. 17.
    Komhyr W D, Waterman L S, Taylor W R. Semiautomatic nondispersive infrared analyzer apparatus for CO2 air sample analyses. J Geophy Res, 1983, 88: 1315–1322CrossRefGoogle Scholar
  18. 18.
    Zhang X C, Cai Y X, Wen Y P, et al. Study of atmospheric carbon dioxide calibration and flask sample analysis system. Meteorol Sci Technol, 2005, 33(6): 538–547Google Scholar
  19. 19.
    World Meteorological Organization. Global Atmosphere Watch. Geneva: WMO, 1993. 86: 1–19Google Scholar
  20. 20.
    Zhou L X, Tang J, Wen Y P. The impact of local winds and long-range transport on the continuous carbon dioxide record at Mount Waliguan, China. Tellus, 2003, 55B:145–158Google Scholar
  21. 21.
    Conway T J, Steele L P, Novelli P C. Correlations among atmospheric CO2, CH4 and CO in the Arctic, March 1989. Atmos Environ, 1993, 27A(17–18): 2881–2894Google Scholar
  22. 22.
    Zhou L X, Li J L, Wen Y P, et al. Background variations of atmospheric carbon dioxide and its stable carbon isotopes at Mt. Waliguan. Acta Sci Circum, 2003, 23(3): 295–300Google Scholar
  23. 23.
    Zhou L X, Thomas J C, James W C, et al. Long-term record of atmospheric CO2 and stable isotopic ratios at Waliguan Observatory: Seasonally averaged 1991–2002 source/sink signals, and a comparison of 1998–2002 record to the 11 selected sites in the Northern Hemisphere. Global biogeochem Cycles, 2006, 20: GB2001, doi: 10.1029/2004GB002431CrossRefGoogle Scholar
  24. 24.
    Cape J N, Methven J, Hudson L E. The use of trajectory cluster analysis to interpret trace gas measurements at Mace Head, Ireland. Atmos Environ, 2000, 34: 351–363CrossRefGoogle Scholar
  25. 25.
    Draxler R R. Description of the HYSPLIT-4 Modeling System. NOAA Technical Memo, ERL ARL224, 1997Google Scholar
  26. 26.
    Miller J B, Tans P P, White W C, et al. The atmospheric signal of terrestrial carbon isotopic discrimination and its implication for partition carbon fluxes. Tellus, 2003, 55: 197–206CrossRefGoogle Scholar

Copyright information

© Science in China Press and Springer Berlin Heidelberg 2009

Authors and Affiliations

  • LiXin Liu
    • 1
  • LingXi Zhou
    • 1
  • XiaoChun Zhang
    • 1
  • Min Wen
    • 1
  • Fang Zhang
    • 1
  • Bo Yao
    • 1
  • ShuangXi Fang
    • 1
  1. 1.Key Laboratory for Atmospheric Chemistry, Centre for Atmosphere Watch and Services (CAWAS)Chinese Academy of Meteorological Sciences (CAMS), China Meteorological Administration (CMA)BeijingChina

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