Articles | Volume 19, issue 11
https://doi.org/10.5194/tc-19-5389-2025
https://doi.org/10.5194/tc-19-5389-2025
Research article
 | 
04 Nov 2025
Research article |  | 04 Nov 2025

Snow particle motion in process of cornice formation

Hongxiang Yu, Li Guang, Benjamin Walter, Jianping Huang, Ning Huang, and Michael Lehning

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Cited articles

Anderson, R. S. and Haff, P. K.: Wind modification and bed response during saltation of sand in air, in: Aeolian grain transport 1, 21–51, Springer, https://doi.org/10.1007/978-3-7091-6706-9_2, 1991. a
Baek, S. J. and Lee, S. J.: A new two-frame particle tracking algorithm using match probability, Experiments in Fluids, 22, https://doi.org/10.1007/BF01893303, 1996. a
Bagnold, R. A.: The physics of blown sand and desert dunes, Courier Corporation, https://doi.org/doi=10.1007/978-94-009-5682-7_2, 2012. a, b
Bartlett, S. J., Rüedi, J.-D., Craig, A., and Fierz, C.: Assessment of techniques for analyzing snow crystals in two dimensions, Annals of Glaciology, 48, 103–112, https://doi.org/10.3189/172756408784700752, 2008. a
Colbeck, S. C.: An overview of seasonal snow metamorphism, Reviews of Geophysics, 20, 45–61, https://doi.org/10.1029/RG020i001p00045, 1982. a
Short summary
Cornices are overhanging snow accumulations that form on mountain crests. Using wind-tunnel experiments and high-speed photography, the study tracks particle trajectories around cornices and finds distinct differences between edge and surface deposition. A static adhesion model for edge deposition was developed and validated to predict how particle size and shape affect adhesion. The work clarifies the microdynamics of early cornice growth and provides a foundation for avalanche modeling.
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