Articles | Volume 11, issue 6
Research article
20 Dec 2017
Research article |  | 20 Dec 2017

The significance of vertical moisture diffusion on drifting snow sublimation near snow surface

Ning Huang and Guanglei Shi

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Revised manuscript not accepted

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Cited articles

Bintanja, R.: Snowdrift suspension and atmospheric turbulence, Part I: Theoretical background and model description, Bound.-Lay. Meteorol., 95, 343–368, 2000.
Bintanja, R.: Snowdrift Sublimation in a Katabatic Wind Region of the Antarctic Ice Sheet, J. Appl. Met., 40, 1952–1966, 2001.
Carrier, C.: On Slow Viscous Flow, Tech. rep., Office of Naval Research, Contract Nonr-653(00), Brown University, Providence, RI, 1953.
Csanady, G. T.: Turbulent Diffusion of Heavy Particles in the Atmosphere, J. Atmos. Sci., 20, 201–208, 1963.
Cullen, N. J., Molg, T., Kaser, G., Steffen, K., Hardy, D. R.: Energy-balance model validation on the top of Kilimanjaro, Tanzania, using eddy covariance data, Ann. Glaciol., 46, 227–233, 2007.
Short summary
Snow is an important part of the cryosphere, and blowing snow sublimation is an important method to change the snow distribution. However, in the previous studies blowing snow sublimation near surface was ignored. Herein, we built a blowing snow sublimation model to study the sublimation in near-surface region. The results showed that the mass of snow sublimation near surface accounted for even more than half of the total. Therefore, blowing snow sublimation near surface cannot be neglected.