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Advances in Atmospheric Sciences

, Volume 22, Issue 5, pp 751–758 | Cite as

HCl quasi-biennial oscillation in the stratosphere and a comparison with ozone QBO

  • Chen Yuejuan
  • Shi Chunhua
  • Zheng Bin
Article

Abstract

HALOE data from 1992 to 2003 are used to analyze the interannual variation of the HCl volume mixing ratio and its quasi-biennial oscillation (QBO) in the stratosphere, and the results are compared with the ozone QBO. Then, the NCAR two-dimensional interactive chemical, dynamical and radiative model is used to study the effects of the wind QBO on the distribution and variation of HCl in the stratosphere. The results show that the QBO signals in the HCl mixing ratio are mainly at altitudes from 50 hPa to 5 hPa; the larger amplitudes are located between 30 hPa and 10 hPa; a higher HCl mixing ratio usually corresponds to the westerly phase of the wind QBO and a lower HCl mixing ratio usually corresponds to the easterly phase of the wind QBO in a level near 20 hPa and below. In the layer near 10 hPa–5 hPa, the phase of the HCl QBO reverses earlier than the phase of the wind QBO; the QBO signals for HCl in the extratropics are also clear, but with reversed phase compared with those over the Tropics. The HCl QBO signals at 30°N are clearer than those at 30°S; the QBOs for HCl and ozone have a similar phase at the 50 hPa-20 hPa level while they are out of phase near 10 hPa; the simulated structures of the HCl QBO agree well with observations. The mechanism for the formation of the HCl QBO and the reason for differences in the vertical structure of the HCl and ozone QBO are attributed to the transport of HCl and ozone by the wind QBO-induced meridional circulation.

Key words

HCl quasi-biennial oscillation stratosphere 

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References

  1. Chen Yuejuan, Zheng Bin, and Zhang Hong, 2002: The features of ozone quasi-biennial oscillation in the tropical stratosphere and its numerical simulation.Adv. Atmos. Sci.,19(5), 777–793.CrossRefGoogle Scholar
  2. Chipperfield, M. P., L. J. Kinnersley, and J. Zawodny, 1994: A two-dimensional model study of the QBO signal in SAGE II NO2 and O3.Geophys. Res. Lett.,21, 589–592.CrossRefGoogle Scholar
  3. Funk, J. P., and G. L. Garnham. 1962: Australian ozone observations and a suggested 24 month cycle.Tellus,14, 378–382.CrossRefGoogle Scholar
  4. Gray, L. J., and M. P. Chipperfield, 1990: On the interannual variability of trace gases in the middle atmosphere.Geophys. Res. Lett.,17, 933–936.CrossRefGoogle Scholar
  5. Gray, L. J., and S. Ruth, 1992: The interannual variability of trace gases in the stratosphere: A comparative study of the LIMS and UARS measurement periods.Geophys. Res. Lett.,19, 673–676.CrossRefGoogle Scholar
  6. Hasebe, F., 1983, Interannual variations of global ozone revealed from Nimbus 4 BUV and ground-based observations.J. Geophys. Res.,88, 6819–6834.CrossRefGoogle Scholar
  7. Huang, T., and Coauthors, 1997: Description of SOCRATES, A chemical, dynamical, radiative 2-D model. Tech. Rept, NCAR, Boulder, Colorado, 88pp.Google Scholar
  8. Luo, M., J. M. Russell III, and T. Y. W. Huang, 1997: Halogen Occultation Experiment observations of the quasi-biennial oscillation and the effects of Pinatubo aerosol in the tropical stratosphere.J. Geophys. Res.,102, 19187–19198.CrossRefGoogle Scholar
  9. Ramanathan, K. R., 1963: Bi-annual variation of atmospheric ozone over the tropics.Quart. J. Roy. Meteor. Soc.,89, 540–542.CrossRefGoogle Scholar
  10. Reed, R. J., W. J. Campbell, L. A. Rasmussen, and D. G. Rogers, 1961: Evidence of downward propagating annual wind reversal in the equatorial Stratosphere.J. Geophys. Res.,66, 813–818.CrossRefGoogle Scholar
  11. Russell, and Coauthors, 1993: The Halogen Occultation Experiment.J. Geophys. Res.,98(D6), 10777–10797.CrossRefGoogle Scholar
  12. Schoeberl, M. R., A. E. Roche, J. M. Russell III, D. Ortland, P. B. Hays, and J. W. Waters, 1997: An eastimation of the dynamical isolation of the tropical lower stratosphere using UARS wind and trace gas observations of the quasi-biennial oscillation.Geophys. Res. Lett.,24, 53–56.CrossRefGoogle Scholar
  13. Veryard, R. G., and R. A. Ebdon, 1991: Fluctuation in tropical stratosphere winds.Meteor. Mag.,90, 125–143.Google Scholar
  14. Yang, H., and K. K. Tung, 1995: On the phase propagation of extratropical ozone quasi-biennial oscillation in observational data.J. Geophys. Res.,100, 9091–9100.CrossRefGoogle Scholar
  15. Zawodny, J. M., and M. P. McCormick, 1991: Stratospheric Aerosol and Gas Experiment II measurements of the quasi-biennial oscillations in ozone and nitrogen dioxide.J. Geophys. Res.,96, 9371–9377.CrossRefGoogle Scholar
  16. Zhang Hong, Chen Yuejuan, and Wu Beiying, 2000: Impact of quasi-biennial oscillation on the distribution of the trace gases in the stratosphere.Chinese J. Atmos. Sci.,24(1), 103–110.Google Scholar

Copyright information

© Advances in Atmospheric Sciences 2003

Authors and Affiliations

  1. 1.School of Earth and Space SciencesUniversity of Science and Technology of ChinaHefei
  2. 2.Institute of Tropical and Marine MeteorologyChina Meteorological AdministrationGuangzhou

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