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Thermal Regime of the Troposphere, Stratosphere, and Lower Mesosphere in the Northern Hemisphere in 1979–2016

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Abstract

The characteristics of spatiotemporal variability of air temperature and ozone mass mixing ratio at 26 levels from the ground to the altitude of 64 km are considered using the ERA-Interim reanalysis data for 1979–2016. Differences are revealed in the distribution of air temperature trends between seasons and latitude zones, between the Atlantic-European, Asian-Pacific, and American sectors of the Northern Hemisphere mid-latitudes, and between the thermal regime over the land and ocean. The correlations between the layers and atmospheric circulation patterns in different seasons are assessed.

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Funding

The research was supported by the Russian Foundation for Basic Research (grants 18-05-00721 and 18-45-160006).

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Authors and Affiliations

  1. Kazan (Volga Region) Federal University, ul. Kremlevskaya 18, Kazan, 420008, Russia

    Yu. P. Perevedentsev, K. M. Shantalinskii & V. V. Gur’yanov

  2. Hydrometeorological Research Center of the Russian Federation, Bolshoi Predtechenskii per. 11-13, Moscow, 123242, Russia

    A. A. Vasil’ev

Authors
  1. Yu. P. Perevedentsev
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  2. K. M. Shantalinskii
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  3. A. A. Vasil’ev
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  4. V. V. Gur’yanov
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Corresponding author

Correspondence to Yu. P. Perevedentsev.

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Russian Text © The Author(s), 2019, published in Meteorologiya i Gidrologiya, 2019, No. 8, pp. 5–20.

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Perevedentsev, Y.P., Shantalinskii, K.M., Vasil’ev, A.A. et al. Thermal Regime of the Troposphere, Stratosphere, and Lower Mesosphere in the Northern Hemisphere in 1979–2016. Russ. Meteorol. Hydrol. 44, 501–512 (2019). https://doi.org/10.3103/S1068373919080016

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  • DOI: https://doi.org/10.3103/S1068373919080016

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