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Snow accumulation on ground and in tree branches in Germany Snow blowing across a highway in Canada Spring snow on a mountain in France. Classifications of snow describe and categorize the attributes of snow-generating weather events, including the individual crystals both in the air and on the ground, and the deposited snow pack as it changes over time.
[10] [11] Powder skis use a design with wide tips and shorter tail lengths. [12] Powder skis typically feature wide tips, ranging from 140 to 155 millimeters. The tails are slightly more tapered, often within a 125- to 140-millimeter range. This design helps powder skis remain buoyant in snow. The contours and proportions of a ski's tip, waist ...
A powder snow avalanche is a type of avalanche where snow grains are largely or completely suspended and moved by air in a state of fluid turbulence. They are particle-laden gravity currents [ 1 ] and closely related to turbidity currents , pyroclastic flows from volcanoes and dust storms in the desert.
If the avalanche moves fast enough some of the snow may mix with the air forming a powder snow avalanche, which is a type of gravity current. They occur in three major mechanisms: [60] Slab avalanches occur in snow that has been deposited, or redeposited by wind. They have the characteristic appearance of a block (slab) of snow cut out from its ...
Snowpack is an accumulation of snow that compresses with time and melts seasonally, often at high elevation or high latitude. [1] [2] Snowpacks are an important water resource that feed streams and rivers as they melt, sometimes leading to flooding. Snowpacks provide water to down-slope communities for drinking and agriculture. [3]
A White House decoration volunteer throws fake snow onto a Christmas tree at the White House. Fake snow is any product which simulates the appearance and texture of snow, without being made from frozen crystalline water. Fake snow has been made from many materials. In the early 1900s, decorative snow was sometimes made from borax flakes and ...
"Sugar snow" as a layer in a snowpack Depth hoar crystals, imaged with light and with scanning electron microscopy Sugar snow - panoramio. Depth hoar, also called sugar snow [1] or temperature gradient snow (or TG snow), [2] are large snow-crystals occurring at the base of a snowpack that form when uprising water vapor deposits, or desublimates, onto existing snow crystals.
The lower end of a glacier is usually free from snow and névé in summer. In the upper end and above the upper boundary of a glacier, the snow field is an ice field covered with snow. The glacier upper boundary, where it emerges from under a snow field, is ill-defined because of gradual transition. [2]