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The rate of bedrock weathering by frost action : field measurements and a predictive model
Principal results of the field measurements (shattering rate, surface temperature, moisture content, and the physical and strength properties of bedrock) conducted in four rockwall sites of the Japanese Alps, Mt. Ainodake, during 1982-1987
. Discussion of the predictive model, which was calibrated using these field data.

Diurnal freeze-thaw depth in rockwalls: field measurements and theoretical considerations
but both diurnal and seasonal freezing occur. Diurnal frost and thaw depths were determined from the field data and compared with the theoretical values calculated by the modified Berggren equation. The seasonal frost depth, which could not be directly
determined from the field data, was also estimated on the basis of the analysis of the diurnal freeze-thaw depths.

The relationship between frost heave and downslope soil movement : field measurements in the Japanese Alps

Field observations of weathering processes and the related landforms, combined with laboratory analyses of weathering products, permit a synthetic evaluation of Late Cenozoic weathering environments in the Sør Rondane Mountains, an arid upland

This paper presents atomated monitoring of rock joint widening and temperatures, in autumn and spring, on 3 rock outcrops around Mount Ainodake, in the Akaishi Range, southern Japanese Alps, where a series of field observations on frost weathering

Microgelivation versus macrogelivation : towards bridging the gap between laboratory and field frost weathering

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