Articles | Volume 18, issue 9
Ann. Geophys., 18, 1145–1153, 2000
https://doi.org/10.1007/s00585-000-1145-0

Special issue: IXe EISCAT

Ann. Geophys., 18, 1145–1153, 2000
https://doi.org/10.1007/s00585-000-1145-0

  30 Sep 2000

30 Sep 2000

Ion-neutral coupling in the high-latitude F-layer from incoherent scatter and Fabry-Perot interferometer measurements

K. Cierpka, M. J. Kosch, M. Rietveld, K. Schlegel, and T. Hagfors K. Cierpka et al.
  • Max-Planck-Institut Aeronomie, 37191 Katlenburg-Lindau, Germany

Abstract. Since the auroral ionosphere provides an important energy sink for the magnetosphere, ionosphere-thermosphere coupling must be investigated when considering the energy budget of the ionosphere-magnetosphere coupling. We present the first Scandinavian ground-based study of high-latitude F-region ion-neutral frictional heating where ion velocity and temperature are measured by the EISCAT incoherent scatter radar as well as neutral wind and temperature being measured simultaneously by a Fabry-Perot interferometer. A geomagnetically active period (Kp = 7 – 5) and quiet period (Kp = 0+ – 0) were studied. Neglecting the neutral wind can result in errors of frictional heating estimates of 60% or more in the F-layer. About 96% of the local ion temperature enhancement over the neutral temperature is accounted for by ion-neutral frictional heating.

Key words: Ionosphere (auroral ionosphere; ionosphere-atmosphere interactions)

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