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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 16, issue 10
Ann. Geophys., 16, 1212–1225, 1998
https://doi.org/10.1007/s00585-998-1212-5
© European Geosciences Union 1998

Special issue: VIIIe EISCAT

Ann. Geophys., 16, 1212–1225, 1998
https://doi.org/10.1007/s00585-998-1212-5
© European Geosciences Union 1998

  31 Oct 1998

31 Oct 1998

Geophysical phenomena during an ionospheric modification experiment at Tromsø, Norway

N. F. Blagoveshchenskaya1, V. A. Kornienko1, A. V. Petlenko1, A. Brekke2, and M. T. Rietveld3 N. F. Blagoveshchenskaya et al.
  • 1Arctic and Antarctic Research Institute (AARI), 199397, St. Petersburg, Russia
  • 2Auroral Observatory, University of Tromsø, N-9037, Tromsø, and The University Courses of Svalbard, Svalbard, Norway
  • 3EISCAT, N-9027 Ramfjørdbotn, Norway

Abstract. We present an analysis of phenomena observed by HF distance-diagnostic tools located in St. Petersburg combined with multi-instrument observation at Tromsø in the HF modified ionosphere during a magnetospheric substorm. The observed phenomena that occurred during the Tromsø heating experiment in the nightside auroral Es region of the ionosphere depend on the phase of substorm. The heating excited small-scale field-aligned irregularities in the E region responsible for field-aligned scattering of diagnostic HF waves. The equipment used in the experiment was sensitive to electron density irregularities with wavelengths 12–15 m across the geomagnetic field lines. Analysis of the Doppler measurement data shows the appearance of quasiperiodic variations with a Doppler frequency shift, fd and periods about 100–120 s during the heating cycle coinciding in time with the first substorm activation and initiation of the upward field-aligned currents. A relationship between wave variations in fd and magnetic pulsations in the Y-component of the geomagnetic field at Tromsø was detected. The analysis of the magnetic field variations from the IMAGE magnetometer stations shows that ULF waves occurred, not only at Tromsø, but in the adjacent area bounded by geographical latitudes from 70.5° to 68° and longitudes from 16° to 27°. It is suggested that the ULF observed can result from superposition of the natural and heater-induced ULF waves. During the substorm expansion a strong stimulated electromagnetic emission (SEE) at the third harmonic of the downshifted maximum frequency was found. It is believed that SEE is accompanied by excitation of the VLF waves penetrating into magnetosphere and stimulating the precipitation of the energetic electrons (10–40 keV) of about 1-min duration. This is due to a cyclotron resonant interaction of natural precipitating electrons (1–10 keV) with heater-induced whistler waves in the magnetosphere. It is reasonable to suppose that a new substorm activation, exactly above Tromsø, was closely connected with the heater-induced precipitation of energetic electrons.

Key words. Ionosphere (active experiments; ionosphere · magnetosphere interactions). Radio science (nonlinear phenomena).

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