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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 17, issue 6
Ann. Geophys., 17, 794–805, 1999
https://doi.org/10.1007/s00585-999-0794-x
© European Geosciences Union 1999
Ann. Geophys., 17, 794–805, 1999
https://doi.org/10.1007/s00585-999-0794-x
© European Geosciences Union 1999

  30 Jun 1999

30 Jun 1999

Vertical circulation and thermospheric composition: a modelling study

H. Rishbeth1 and I. C. F. Müller-Wodarg2,1 H. Rishbeth and I. C. F. Müller-Wodarg
  • 1Department of Physics and Astronomy, University of Southampton, Southampton SO17 1BJ, UK
  • 2Atmospheric Physics Laboratory, Department of Physics and Astronomy, University College London, 67-73 Riding House Street, London W1P 7PP, UK

Abstract. The coupled thermosphere-ionosphere-plasmasphere model CTIP is used to study the global three-dimensional circulation and its effect on neutral composition in the midlatitude F-layer. At equinox, the vertical air motion is basically up by day, down by night, and the atomic oxygen/molecular nitrogen [O/N2] concentration ratio is symmetrical about the equator. At solstice there is a summer-to-winter flow of air, with downwelling at subauroral latitudes in winter that produces regions of large [O/N2] ratio. Because the thermospheric circulation is influenced by the high-latitude energy inputs, which are related to the geometry of the Earth's magnetic field, the latitude of the downwelling regions varies with longitude. The downwelling regions give rise to large F2-layer electron densities when they are sunlit, but not when they are in darkness, with implications for the distribution of seasonal and semiannual variations of the F2-layer. It is also found that the vertical distributions of O and N2 may depart appreciably from diffusive equilibrium at heights up to about 160 km, especially in the summer hemisphere where there is strong upwelling.

Atmospheric composition and structure (thermosphere · composition and chemistry) · Ionosphere (ionosphere · atmosphere interactions)

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