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Snowpack is an accumulation of snow that compresses with time and melts seasonally, often at high elevation or high latitude. 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. High-latitude or high-elevation snowpacks contribute mass to in their accumulation zones, where annual snow deposition exceeds annual melting.
Assessing the formation and stability of snowpacks is important in the study and prediction of .9781594851292, Mountaineers Books. . ISBN 9781594851292Tobias Kurzeder, Holger Feist, Powderguide: Managing Avalanche Risk, Mountain Sports Press, 978-0972482738, 190 pages Scientists study the physical properties of snow under different conditions and their evolution, and more specifically snow metamorphism,Pinzer, B. R., Schneebeli, M., and Kaempfer, T. U.(2012) " Vapor flux and recrystallization during dry snow metamorphism under a steady temperature gradient as observed by time-lapse micro-tomography", TheCryosphere, 6, 1141–1155, snow hydrology (that is, the contribution of snow melt to catchment hydrology), the evolution of snow cover with climate change and its effect on the ice–albedo feedback and hydrology, both on the ground and by using remote sensing. (2025). 9781509033324 ISBN 9781509033324 Snow is also studied in a more global context of impact on animal and plant succession. An important effort is put into snow classification, both as a hydrometeor and on the ground.
Maritime snowpacks are typically found on the windward side of continents, near oceans. They usually feature warmer winter temperatures that stay around freezing () and more precipitation, leading to a snowpack that is over deep. Frequent storms deposit snow with a higher snow-water equivalent, often around 10 to 20 percent moisture. Most avalanches occur during or immediately after storms, as weak layers do not persist with warmer temperatures and frequent midwinter rain. Thus, it is typical to ski steep, avalanche prone terrain as soon as 24 to 36 hours after the storm. Many areas with a maritime snowpack receive of annual snowfall. Areas with a typically maritime snowpack include the Cascade Range, Coastal Range, western Norway, and the Sierra Nevada.
Intermountain or transitional snowpack is colder and drier than maritime snowpack, usually around deep. Temperatures stay colder than maritime climates but warmer than continental climates, around . Although intermountain snowpacks can feature persistent weak layers, avalanches also occur within storm snow. Unlike in maritime climates, instability lingers for several days to weeks after storms. Typical areas for this snowpack include the Wasatch Range, Selkirks, and parts of the Alps.
Continental snowpacks are the coldest and thinnest, featuring snow less than deep and winter temperatures under . Storms are less frequent and deposit less snow, which is less dense. Faceted snow and depth hoar is the typical weak layer, often covered by hard wind slabs. The instability is very persistent and often leads to higher rates of avalanche fatalities. Areas with a typically continental snowpack include Colorado, the Canadian Rockies, the Brooks Range, and the Pamir Mountains. Because of the persistence of weak layers, forecasting relies much more heavily on snowpit tests to determine stability. In continental climates, avalanches can start on less steep slopes than in intermountain or maritime climates.
Local and regional weather conditions can change the type of snowpack typical for a region, for example a typically maritime region might have a cold and thin early season snowpack that resembles continental type, while even a few feet apart the snowpack depth can vary enough to produce vastly different conditions. Elevation also dramatically affects the type of avalanches typically experienced in a particular area.
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