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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 7, issue 8
Atmos. Chem. Phys., 7, 2047-2055, 2007
https://doi.org/10.5194/acp-7-2047-2007
© Author(s) 2007. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.
Atmos. Chem. Phys., 7, 2047-2055, 2007
https://doi.org/10.5194/acp-7-2047-2007
© Author(s) 2007. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.

  24 Apr 2007

24 Apr 2007

Definition of "banner clouds" based on time lapse movies

J. H. Schween1, J. Kuettner2, D. Reinert3, J. Reuder4, and V. Wirth3 J. H. Schween et al.
  • 1currently at: Institute for Geophysics and Meteorology, University of Cologne, Germany
  • 2National Center for Atmospheric Research, Boulder, CO, USA
  • 3Institute for Atmospheric Physics, Johannes Gutenberg-University, Mainz, Germany
  • 4Geophysical Institute, University of Bergen, Norway

Abstract. Banner clouds appear on the leeward side of a mountain and resemble a banner or a flag. This article provides a comprehensive definition of "banner clouds". It is based primarily on an extensive collection of time lapse movies, but previous attempts at an explanation of this phenomenon are also taken into account. The following ingredients are considered essential: the cloud must be attached to the mountain but not appear on the windward side; the cloud must originate from condensation of water vapour contained in the air (rather than consist of blowing snow); the cloud must be persistent; and the cloud must not be of convective nature. The definition is illustrated and discussed with the help of still images and time lapse movies taken at Mount Zugspitze in the Bavarian Alps.

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