Many studies have been conducted on the friction of ice and snow, and several theories have been proposed, including pressure
melting, frictional melting, adhesion, and pseudo-liquid film lubrication. However, each theory has its own issues, and no
satisfactory theory that can rationally explain the slipperiness of ice has yet been established. In this study, many previous reports
on the friction of ice and snow were investigated, and the following new friction model was proposed. That is, in the friction
between the ice particle and the slider, the adhesion area of the ice particle undergo plastic deformation and become high
temperature, generating high-pressure water vapor and water. The generation of water vapor and water eliminates the contact area
between the ice particle and the slider, significantly reducing the shear stress on the friction surface. This phenomenon occurs
continuously on the friction surface, resulting in a low coefficient of friction. By adopting this water vapor generation model, it
became possible to rationally explain the friction characteristics of ice and snow, and also to resolve issues with previous theories.
Furthermore, this model provides a reasonable explanation for why soft materials like rubber exhibit a high coefficient of friction
against ice and snow.
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