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_____________________________________________________ Institute for Optical Monitoring SB RAS

Ippolitov I. I., Kabanov M. V. , Komarov A. I., Kuskov A. I., Loginov S. V., Smirnov S. V. Structure and D ynamics of G round T emperature and P ressure F ields in Asian P art of Russia.

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_____________________________________________________ Institute for Optical Monitoring SB RAS

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  1. Ippolitov I. I., Kabanov M. V., Komarov A. I.,Kuskov A. I., Loginov S. V., SmirnovS. V. Structure and Dynamics of Ground Temperature and Pressure Fields inAsian Part of Russia International Conference and Young Scientists School on Computational Information Technologies for Environmental Sciences Tomsk, Russia, September 1-11, 2003 _____________________________________________________ Institute for Optical Monitoring SB RAS 10/3, Akademicheskii Ave., Tomsk 634055, Russia +7-3822-25-89-44, 25-96-81 ceo@iom.tomsknet.ru, sceo@iom.tomsknet.ru

  2. Resolution into components of temporal series

  3. Wavelet analysis of temporal series

  4. Long-term means of surface temperature (°C)

  5. Ranges of seasonal trend of surface temperature (°C)

  6. Long-term trends of surface temperature (°C per decade)

  7. Long-term means of surface pressure (hPa)

  8. Ranges of seasonal trend of surface pressure (hPa)

  9. Long-term trends of surface pressure (hPa per decade)

  10. Correlation between long-term monthly deviations of surface temperature and pressure

  11. Correlation between long-term deviations of surface temperature and pressure in July

  12. Correlation between long-term deviations of surface temperature and pressure in January

  13. Results of wavelet analysis for surface temperature at Omsk

  14. Results of wavelet analysis for surface pressure at Omsk

  15. Correlation between long-term monthly means of surface temperature and pressure according to oscillation periods for 30–40th years to 1995 at the former USSR

  16. Standard deviations (as in previous slide)

  17. Amount of days per year with different types of atmospheric circulation in the Northern hemisphere: 1 – zonal, 2 – un-zonal, 3 – north meridional, 4 – south meridional (climatic trends and 11-years oscillations are also shown) Day 3 Byshev et al. Doklady Earth Sci., 385, 5, 538 (2002) 2 4 1 Year

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