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Variations in temperature at different isobaric levels of the atmosphere, according to data on cosmic rays

  • Proceedings of the 33rd National Conference on Cosmic Rays
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Bulletin of the Russian Academy of Sciences: Physics Aims and scope

Abstract

Temporal variations in the intensity of cosmic rays occur when effects of different natures (including atmospheric effects) coincide. The latter are primarily due to changes in the temperature and density of the atmosphere. One way of obtaining information on variations in temperature at different isobaric levels of the atmosphere using data on the continuous registration of cosmic rays is shown.

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Authors and Affiliations

  1. Geophysical Survey, Siberian Branch, Russian Academy of Sciences, Novosibirsk, 630090, Russia

    V. L. Yanchukovsky, S. A. Sunyakov & V. S. Kuzmenko

Authors
  1. V. L. Yanchukovsky
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  2. S. A. Sunyakov
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  3. V. S. Kuzmenko
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Corresponding author

Correspondence to V. L. Yanchukovsky.

Additional information

Original Russian Text © V.L. Yanchukovsky, S.A. Sunyakov, V.S. Kuzmenko, 2015, published in Izvestiya Rossiiskoi Akademii Nauk. Seriya Fizicheskaya, 2015, Vol. 79, No. 5, pp. 721–723.

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Yanchukovsky, V.L., Sunyakov, S.A. & Kuzmenko, V.S. Variations in temperature at different isobaric levels of the atmosphere, according to data on cosmic rays. Bull. Russ. Acad. Sci. Phys. 79, 667–669 (2015). https://doi.org/10.3103/S1062873815050445

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  • DOI: https://doi.org/10.3103/S1062873815050445

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