Ukrainian Antarctic Journal

No 3 (2005): Ukrainian Antarctic Journal
Articles

Planetary distribution of Geomagnetic Substorms and their Peculiarities in conjugate places

L. N. Yaremenko
S. I. Subbotin Institute of geophysics of NAS of Ukraine, Kyiv
T. A. Mozgovaya
S. I. Subbotin Institute of geophysics of NAS of Ukraine, Kyiv
V.G. Bahmutov
S. I. Subbotin Institute of Geophysics of NAS of Ukraine, Kyiv
Published December 15, 2005
Keywords
  • magnetic substorm,
  • magnetosphere,
  • latitudinal and longitudinal dependence
How to Cite
Yaremenko, L. N., Mozgovaya, T. A., & Bahmutov, V. (2005). Planetary distribution of Geomagnetic Substorms and their Peculiarities in conjugate places. Ukrainian Antarctic Journal, (3), 27-35. https://doi.org/10.33275/1727-7485.3.2005.563

Abstract

A comparison of magnetic substorms at the station Akademik Vernadsky, in Greenland, Japan and New Zealand detected seasonal dependence of the substorms amplitude  with maximum in the lokal winter regardless of a hemisphere. The differences are so great that the disappearance of substorms is observed in the opposite hemisphere in the local summer. Simultaneous appearance of substorms over the globe is observed as well as the amplitude and record form dependence on the longitude and local conditions. The latitudinal dependence of substorm amplitudes are given. Magnetic substorm characteristics obtained in the  Vernadsky station are presented. In general, according to the characteristics of the substorms, they are of the mid-latitudinal type. The events of the southern polar jet approach to Vernadsky station are considered separately. Examples of the same, opposed and disagreeing substorm current directions observed at  Vernadsky station and in North America are shown as well. The substorm origin dependence on the changes of the Bx and By components of the interplanetary magnetic field, its total value B and abrupt, variations of the solar wind velocity and pressure is marked.

References

  1. Yaremenko, L.N., Mischenko, Yu.P., & Mozgovaia, T.A. (1998). Variacii magnitnogo polia v poliarnyh oblastiah [Variations of the magnetic field in the polar regions]. Geofizicheskii zhurnal, 20(6), 40-44. (In Russian)
  2. Yaremenko, L.N., Bakhmutov, V.G., & Mischenko, Yu.P. (1998). Nekotorye dannye o magnitnyh subburiah v Antarktike [Some data about the magnetic substorms in Antarctica]. Bulleten UAC, 2, 133-138. (In Russian)
  3. Yaremenko, L.N., & Mozgovaia, T.A. (2004). Sopriazhennost magnitnyh subbur v srednih shyrotah severnogo i yuzhnogo polushariy [The conjugacy of magnetic substorms in the middle latitudes of the Northern and Southern hemispheres]. Kosmichna nauka i tehnologia, 10(5/6), 105-109. (In Russian)
  4. Yaremenko, L.N., & Melnik, G.V. (2004). Magnitnye buri v ekvatorialnom poiase i poliarnyh oblastiah [Magnetic storms in the equatorial belt and polar regions]. Kosmichna nauka i tehnologia, 10(5/6), 109-115. (In Russian)
  5. Baker, K.B., Greenwald, R.A., Ruohoniemi, J.M. et al. (1989). 1989 PACE. Polar Anglo-American Conjugate Experiment.