(1) Climatic snowline: lowest altitude of a continuous layer of snow on the high mountains in summer. (2) Orographic snowline: lowest altitude at which snow persists on the land surface as isolated co
verings on the mountains in summer.
A special device used to mark the surface between old and new snow. It consists of a piece of white duck 28 inches square, having in each corner triangular pockets in which are inserted slats placed d
iagonally to keep the mat taut and flat.
The transformation that the snow undergoes in the period from deposition to either melting or passage to glacial ice. Meteorological conditions as well as mechanical or gravitational stresses are the
primary external factors that affect snow metamorphism. Dry snow metamorphism is governed by both equilibrium and kinetic growth. In presence of liquid water snow transformation is driven by wet snow metamorphism. In English, snow metamorphism is sometimes and incorrectly called snowmetamorphosis.
The depth of snow in centimetres (cm) on the ground. The total depth of snow on the ground at the time of the observation is determined in whole centimetres by making a series of measurements and taki
ng the average.