Solar-Terrestrial Physics (Dec 2018)

Changes in the middle and upper atmosphere parameters during the January 2013 sudden stratospheric warming

  • Yasyukevich A.S.,
  • Klimenko M.V.,
  • Kulikov Yu.Yu.,
  • Klimenko V.V.,
  • Bessarab F.S.,
  • Korenkov Yu.N.,
  • Marichev V.N.,
  • Ratovsky K.G.,
  • Kolesnik S.A.

DOI
https://doi.org/10.12737/stp-44201807
Journal volume & issue
Vol. 4, no. 4
pp. 48 – 58

Abstract

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We present the results of complex obser-vations of various parameters of the middle and upper atmosphere over Siberia in December 2012 – January 2013, during a major sudden stratospheric warming (SSW) event. We analyze variations in ozone concentration from microwave measurements, in stratosphere and lower mesosphere temperatures from lidar and satellite measurements, in the F2-layer critical frequency (foF2), in the total electron content (TEC), as well as in the ratio of concentrations of atomic oxygen to molecular nitrogen (O/N2) in the thermosphere. To interpret the observed disturbances in the upper atmosphere, the experimental measurements are compared with the results of model calculations obtained with the Global Self-consistent Model of Thermosphere—Ionosphere—Protonosphere (GSM TIP). The response of the upper atmosphere to the SSW event is shown to be a decrease in foF2 and TEC during the evolution of the warming event and a prolonged increase in O/N2, foF2, and TEC after the SSW maximum. For the first time, we observe the relation between the increase in stratospheric ozone, thermospheric O/N2, and ionospheric electron density for a fairly long time (up to 20 days) after the SSW maximum at midlatitudes.

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