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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 15, issue 8
Ann. Geophys., 15, 1037–1047, 1997
https://doi.org/10.1007/s00585-997-1037-7
© European Geosciences Union 1997
Ann. Geophys., 15, 1037–1047, 1997
https://doi.org/10.1007/s00585-997-1037-7
© European Geosciences Union 1997

  31 Aug 1997

31 Aug 1997

The small-scale structure of VHF mesospheric summer echo layers observed at mid-latitudes

D. A. Hooper and L. Thomas D. A. Hooper and L. Thomas
  • Department of Physics, University of Wales, Aberystwyth, SY23 3Bz, UK

Abstract. The VHF radar system at Aberystwyth (52.4° N, 4.1°E) has been used to make high-time-resolution, multi-beam observations of mesospheric summer echo layers. These show that the altitude and the sense of vertical movement of the layers can vary over time-scales of minutes and horizontal scales of kilometres. In general, the altitude profiles of signal-to-noise ratio provide evidence of a bifurcated structure with sharp changes in the horizontal wind vector and vertical velocity, and enhanced spectral width occurring at the bifurcation level. The implications of the small-scale structure for studies of the aspect sensitivity of radar returns are discussed, and the changes in wind-field at the bifurcation level are compared with 'wind corners' observed in rocket studies of the mesosphere at polar latitudes.

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