

Author: Matsushita Hiroki Matsuzawa Masaru Abe Osamu
Publisher: International Glaciological Society
ISSN: 1727-5644
Source: Annals of Glaciology, Vol.53, Iss.61, 2012-12, pp. : 31-38
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Abstract
An experiment using artificial snow was conducted to clarify the influences of temperature and normal load on temporal variations in the shear strength of snow. Artificial snow consisting of dendritic crystals was allowed to accumulate to ∼60 cm depth for the experiment. The shear strength, temperature and weight of the overlying snow were measured at three different depths in the accumulated snow. For the measurement of shear strength, the shear frame index (SFI) was found using a shear frame by placing weights with different masses on the snow contained within the frame. The measured SFI values were treated with the Mohr–Coulomb failure criterion to find the snow cohesion factor
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