Articles | Volume 6, issue 12
Atmos. Chem. Phys., 6, 5307–5314, 2006
https://doi.org/10.5194/acp-6-5307-2006
Atmos. Chem. Phys., 6, 5307–5314, 2006
https://doi.org/10.5194/acp-6-5307-2006

  23 Nov 2006

23 Nov 2006

Isolated lower mesospheric echoes seen by medium frequency radar at 70° N, 19° E

C. M. Hall1, A. H. Manson2, C. E. Meek2, and S. Nozawa3 C. M. Hall et al.
  • 1Tromsø Geophysical Observatory, University of Tromsø, Tromsø, Norway
  • 2Institute of Space and Atmospheric Studies, University of Saskatchewan, Saskatoon, Canada
  • 3The Solar-Terrestrial Environment Laboratory, Nagoya University, Nagoya, Japan

Abstract. We have noted sporadic instances of strong isolated reflections of medium frequency (MF) radar waves from the mesosphere from as low as 50 km altitude and have devised a set of criteria for isolating these apparently anomalous echoes from those normally occurring from progressive partial reflections in the D-region. The object of this study is to map the occurrences of such echoes facilitating comparisons with other observations. For example, the similarity and simultaneity of the echo structure for the 20 January 2005 with VHF radar results presented by Lübken et al. (2006) are particularly striking. In presenting a number of such echo events since 2001 selected from the MF radar dataset (which spans 1997 to present), we find that virtually all echo occurrences coincide with enhanced solar proton fluxes suggesting that substantial ionisation of the mesosphere is a necessary condition. Strong partial reflections of the radio wave in the lower mesosphere combined with seasonally varying total absorption higher up, thus giving false impressions of lower mesospheric layers preferentially in winter, constitute a scenario consistent with our observations.

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