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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 9, issue 6 | Copyright
Atmos. Chem. Phys., 9, 1847-1862, 2009
https://doi.org/10.5194/acp-9-1847-2009
© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.

  16 Mar 2009

16 Mar 2009

Large surface radiative forcing from topographic blowing snow residuals measured in the High Arctic at Eureka

G. Lesins1, L. Bourdages1, T. J. Duck1, J. R. Drummond1, E. W. Eloranta2, and V. P. Walden3 G. Lesins et al.
  • 1Department of Physics and Atmospheric Science, Dalhousie University, Halifax, Canada
  • 2Space Science and Engineering Center, University of Wisconsin, Madison, USA
  • 3Department of Geography, University of Idaho, Moscow, Idaho, USA

Abstract. Ice crystals, also known as diamond dust, are suspended in the boundary layer air under clear sky conditions during most of the Arctic winter in Northern Canada. Occasionally ice crystal events can produce significantly thick layers with optical depths in excess of 2.0 even in the absence of liquid water clouds. Four case studies of high optical depth ice crystal events at Eureka in the Nunavut Territory of Canada during the winter of 2006/07 are presented. They show that the measured ice crystal surface infrared downward radiative forcing ranged from 8 to 36 W m−2 in the wavelength band from 5.6 to 20 μm for 532 nm optical depths ranging from 0.2 to 1.7. MODIS infrared and visible images and the operational radiosonde wind profile were used to show that these high optical depth events were caused by surface snow being blown off 600 to 800 m high mountain ridges about 20 to 30 km North-West of Eureka and advected by the winds towards Eureka as they settled towards the ground within the highly stable boundary layer. This work presents the first study that demonstrates the important role that surrounding topography plays in determining the occurrence of high optical depth ice crystal events from residual blowing snow that becomes a source of boundary layer ice crystals distinct from the classical diamond dust phenomenon.

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