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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 26, issue 5
Ann. Geophys., 26, 1071–1081, 2008
https://doi.org/10.5194/angeo-26-1071-2008
© Author(s) 2008. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Atmospheric studies by optical methods

Ann. Geophys., 26, 1071–1081, 2008
https://doi.org/10.5194/angeo-26-1071-2008
© Author(s) 2008. This work is distributed under
the Creative Commons Attribution 3.0 License.

  28 May 2008

28 May 2008

A case study of a sporadic sodium layer observed by the ALOMAR Weber Na lidar

H. Nesse1,2, D. Heinrich1, B. Williams3, U.-P. Hoppe1, J. Stadsnes2, M. Rietveld4, W. Singer5, U. Blum1,6, M. I. Sandanger2, and E. Trondsen7 H. Nesse et al.
  • 1Norwegian Defence Research Establishment, Kjeller, Norway
  • 2University of Bergen, Department of Physics and Technology, Bergen, Norway
  • 3NorthWest Research Associates/Colorado Research Associates Division, Boulder, USA
  • 4EISCAT Scientific Association, Tromsø, Norway
  • 5Leibniz Institute for Atmospheric Physics, Kühlungsborn, Germany
  • 6Fraunhofer Institute for Technological Trend Analysis, Euskirchen, Germany
  • 7University of Oslo, Department of Physics, Oslo, Norway

Abstract. Several possible mechanisms for the production of sporadic sodium layers have been discussed in the literature, but none of them seem to explain all the accumulated observations. The hypotheses range from direct meteoric input, to energetic electron bombardment on meteoric smoke particles, to ion neutralization, to temperature dependent chemistry. The varied instrumentation located on Andøya and near Tromsø in Norway gives us an opportunity to test the different theories applied to high latitude sporadic sodium layers. We use the ALOMAR Weber sodium lidar to monitor the appearance and characteristics of a sporadic sodium layer that was observed on 5 November 2005. We also monitor the temperature to test the hypotheses regarding a temperature dependent mechanism. The EISCAT Tromsø Dynasonde, the ALOMAR/UiO All-sky camera and the SKiYMET meteor radar on Andøya are used to test the suggested relationships of sporadic sodium layers and sporadic E-layers, electron precipitation, and meteor deposition during this event. We find that more than one candidate is eligible to explain our observation of the sporadic sodium layer.

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