Snowpack

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Digging a snowpit on Taku Glacier, in Alaska to measure snowpack depth and density Snowpitglacier.jpg
Digging a snowpit on Taku Glacier, in Alaska to measure snowpack depth and density

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] High-latitude or high-elevation snowpacks contribute mass to glaciers in their accumulation zones, where annual snow deposition exceeds annual melting. [4]

Contents

Assessing the formation and stability of snowpacks is important in the study and prediction of avalanches. [5] [6] Scientists study the physical properties of snow under different conditions and their evolution, and more specifically snow metamorphism, [7] [8] 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. [9] Snow is also studied in a more global context of impact on animal habitats and plant succession. [10] An important effort is put into snow classification, both as a hydrometeor [11] and on the ground. [12]

Scientific applications

Graph of changing Wyoming Snowpack WY Snowpack.png
Graph of changing Wyoming Snowpack

Snowpack modeling is done for snow stability, flood forecasting, water resource management, and climate studies. [13] Snowpack modeling is either done by simple, statistical methods such as degree day or complex, physically based energy balance models such as SNOWPACK, CROCUS or SNOWMODEL. [14] [15] [16]

Types

Maritime snowpacks typically feature very deep snow as seen at this creek in Washington Dicks Creek 43624.JPG
Maritime snowpacks typically feature very deep snow as seen at this creek in Washington
Less snow is typical for continental snowpacks. Loveland Pass, Colorado Continental divide on Loveland pass 3654 m.jpg
Less snow is typical for continental snowpacks. Loveland Pass, Colorado

The three main types of snowpack are maritime, intermountain, and continental.

Maritime snowpacks are typically found on the windward side of continents, near oceans. They usually feature warmer winter temperatures that stay around freezing (−5 to 5 °C (20 to 40 °F)) and more precipitation, leading to a snowpack that is over 3 metres (10 ft) 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. [17] Thus, it is typical to ski steep, avalanche prone terrain as soon as 24 to 36 hours after the storm. [18] Many areas with a maritime snowpack receive 15 to 25 metres (49 to 82 ft) of annual snowfall. Areas with a typically maritime snowpack include the Cascade Range, Coastal Range, western Norway, [19] and the Sierra Nevada. [18]

Intermountain [20] or transitional [19] snowpack is colder and drier than maritime snowpack, usually around 1.5 to 3 metres (5 to 10 ft) deep. Temperatures stay colder than maritime climates but warmer than continental climates, around −15 to 3 °C (5 to 40 °F). 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. [20] Typical areas for this snowpack include the Wasatch Range, Selkirks, and parts of the Alps. [21]

Continental snowpacks are the coldest and thinnest, featuring snow less than 1.5 metres (5 ft) deep and winter temperatures under −10 °C (10 °F). 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. [22] 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. [19] In continental climates, avalanches can start on less steep slopes than in intermountain or maritime climates. [23]

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. [24] Elevation also dramatically affects the type of avalanches typically experienced in a particular area. [21]

Ecology

Snowpack can affect ecological interactions in boreal and montane forests. In the inland rainforests of British Columbia, for example, deep snowpacks lift caribou into the lower tree canopy while also catching large amounts of fallen "hair" lichens such as Bryoria and Alectoria . These accumulations provide a dependable winter food supply for the endangered deep-snow mountain caribou, a process researchers have termed the "manna effect". [25]

See also

References

  1. ↑ "Definition of SNOWPACK". www.merriam-webster.com. 2024-02-25. Retrieved 2024-03-07.
  2. ↑ "Definition of 'snowpack'". Collins English Dictionary. Retrieved 2024-03-06.
  3. ↑ "Snowpack". education.nationalgeographic.org. Retrieved 2024-03-07.
  4. ↑ "Science of Glaciers". National Snow and Ice Data Center. Retrieved 2024-03-07.
  5. ↑ Cox, Steven M.; Fulsaas, Kris. Mountaineering. Mountaineers Books. pp. 346–347. ISBN   9781594851292.
  6. ↑ Tobias Kurzeder, Holger Feist, Powderguide: Managing Avalanche Risk, Mountain Sports Press, 978-0972482738, 190 pages
  7. ↑ 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, doi : 10.5194/tc-6-1141-2012
  8. ↑ Lehning, Michael. "Fresh insights into snow metamorphism". WSL Institute for Snow and Avalanche Research SLF. Archived from the original on Sep 4, 2017.
  9. ↑ Mousavi, Seyedmohammad (2016). "Dry snowpack and freshwater icepack remote sensing using wideband Autocorrelation radiometry". 2016 IEEE International Geoscience and Remote Sensing Symposium (IGARSS). pp. 5288–5291. doi:10.1109/IGARSS.2016.7730377. ISBN   978-1-5090-3332-4. S2CID   23975901.
  10. ↑ Santeford, Henry S.; Smith, James Leroy (January 1974). Advanced Concepts and Techniques in the Study of Snow and Ice Resources: An Interdisciplinary Symposium; [papers]. National Academy of Sciences. p. 273. ISBN   9780309022354.
  11. ↑ Libbrecht, Kenneth G. "Snowflakes and Snow Crystals". www.its.caltech.edu.
  12. ↑ "IACS". www.cryosphericsciences.org.
  13. ↑ Oliver, John E. (2008-04-23). Encyclopedia of World Climatology. Springer. p. 660. ISBN   9781402032646.
  14. ↑ Morin, Samuel; Horton, Simon; Techel, Frank; Bavay, Mathias; Coléou, Cécile; Fierz, Charles; Gobiet, Andreas; Hagenmuller, Pascal; Lafaysse, Matthieu; Ližar, Matjaž; Mitterer, Christoph; Monti, Fabiano; Müller, Karsten; Olefs, Marc; Snook, John S. (2020-02-01) [2019-10-30]. "Application of physical snowpack models in support of operational avalanche hazard forecasting: A status report on current implementations and prospects for the future". Cold Regions Science and Technology. 170 (published 2019-10-30): 102910. doi: 10.1016/j.coldregions.2019.102910 .
  15. ↑ Viallon-Galinier, Léo; Hagenmuller, Pascal; Lafaysse, Matthieu (2020-12-01). "Forcing and evaluating detailed snow cover models with stratigraphy observations". Cold Regions Science and Technology. 180: 103163. Bibcode:2020CRST..18003163V. doi: 10.1016/j.coldregions.2020.103163 . ISSN   0165-232X.
  16. ↑ Liston, Glen E.; Elder, Kelly (2006). "A distributed snow-evolution modeling system (SnowModel)". Journal of Hydrometeorology. 7 (6): 1259–1276. Bibcode:2006JHyMe...7.1259L. doi:10.1175/JHM548.1.
  17. ↑ Tremper 2018, Maritime—Mountains Bordering Oceans.
  18. 1 2 Volken, Martin; Schell, Scott; Wheeler, Margaret (2007). Backcountry Skiing: Skills for Ski Touring and Ski Mountaineering. The Mountaineers Books. p. 98. ISBN   978-1-59485-250-3.
  19. 1 2 3 McClung & Schaerer 2006, p. 22.
  20. 1 2 Tremper 2018, Intermountain—Mountains with an Intermediate Influence of Oceans.
  21. 1 2 McClung & Schaerer 2006, p. 23.
  22. ↑ Tremper 2018, Continental—Mountains Far from the Influence of Oceans.
  23. ↑ Tremper, Bruce (2013). Avalanche Essentials: A Step-by-Step System for Safety and Survival. Slope steepness of avalanches by climate: Mountaineers Books. ISBN   978-1-59485-718-8.
  24. ↑ Tremper 2018, Avalanche climates.
  25. ↑ Goward, Trevor; Coxson, Darwyn; Gauslaa, Yngvar (2024). "The Manna Effect – a review of factors influencing hair lichen abundance for Canada's endangered Deep-Snow Mountain Caribou (Rangifer arcticus montanus)". The Lichenologist. 56 (4): 121–135. doi: 10.1017/S0024282924000161 .

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