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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 15, issue 12
Ann. Geophys., 15, 1595–1603, 1997
https://doi.org/10.1007/s00585-997-1595-8
© European Geosciences Union 1997
Ann. Geophys., 15, 1595–1603, 1997
https://doi.org/10.1007/s00585-997-1595-8
© European Geosciences Union 1997

  31 Dec 1997

31 Dec 1997

The sunspot cycle, the QBO, and the total ozone over Northeastern Europe: a connection through the dynamics of stratospheric circulation

B. Soukharev B. Soukharev
  • Department of Climatology, St.-Petersburg State University, 10 linia, 33, St.-Petersburg, 199178, Russia
  • E-mail: BORIS@SEB.USR.PU.RU

Abstract. The interaction between the factors of the quasi-biennial oscillation (QBO) and the 11-year solar cycle is considered as an separate factor influencing the interannual January-March variations of total ozone over Northeastern Europe. Linear correlation analysis and the running correlation method are used to examine possible connections between ozone and solar activity at simultaneous moment the QBO phase. Statistically significant correlations between the variations of total ozone in February and, partially, in March, and the sunspot numbers during the different phases of QBO are found. The running correlation method between the ozone and the equatorial zonal wind demonstrates a clear modulation of 11-y solar signal for February and March. Modulation is clearer if the QBO phases are defined at the level of 50 hPa rather than at 30 hPa. The same statistical analyses are conducted also for possible connections between the index of stratospheric circulation C1 and sunspot numbers considering the QBO phase. Statistically significant connections are found for February. The running correlations between the index C1 and the equatorial zonal wind show the clear modulation of 11-y solar signal for February and March. Based on the obtained correlations between the interannual variations of ozone and index C1, it may be concluded that a connection between solar cycle – QBO – ozone occurs through the dynamics of stratospheric circulation.

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