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

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...

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Bibliographic Details
Published in:Atmospheric Chemistry and Physics
Main Authors: Lesins, G., Bourdages, L., Duck, T. J., Drummond, J. R., Eloranta, E. W., Walden, V. P.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/acp-9-1847-2009
https://www.atmos-chem-phys.net/9/1847/2009/