Skip to content
snow

File:CargoNet_Di_12_Euro_4000_Lønsdal_-_Bolna.jpg · Wikimedia Commons · See Wikimedia Commons

EntityQ7561· pop 228· linked from 2,255 articles

Also known as snowfall, snowfalls

Snow consists of individual ice crystals that grow while suspended in the atmosphere—usually within clouds—and then fall, accumulating on the ground where they undergo further changes. It consists of frozen crystalline water throughout its life cycle, starting when, under suitable conditions, the ice crystals form in the atmosphere, increase to millimeter size, precipitate and accumulate on surfaces, then metamorphose in place, and ultimately melt, slide, or sublimate away.

AI overview

Snow is frozen water that forms as ice crystals in clouds, grows larger, and falls to accumulate on the ground, where it continues to change over time. It matters because it represents a significant part of Earth's water cycle, undergoing transformations from its initial crystalline formation through melting, sliding, or evaporation.

AI-generated from the Wikipedia summary — may contain errors.

Key facts

Material.name
Snow
Material.image
CargoNet Di 12 Euro 4000 Lønsdal - Bolna.jpg
Material.caption
Norwegian train plowing through drifted snow
Material.density
0.1–0.8 g/cm3
Material.tensile_strength
1.5–3.5 kPa
Material.compressive_strength
3–7 MPa
Material.melting_point
0 °C
Material.thermal_conductivity_note
For densities 0.1 to 0.5 g/cm3
Material.thermal_conductivity
0.05–0.7 W/(K·m)
Material.dielectric_constant_note
For dry snow density 0.1 to 0.9 g/cm3
Material.dielectric_constant
1–3.2
Material.footnotes
The physical properties of snow vary considerably from event to event, sample to sample, and over time.
Material.image_size
300px

via Wikipedia infobox

Research

21,551 papers

via PubMed

Wikidata facts

Image
Düsseldorf Hofgarten 2009.jpg
Show 4 more facts
Commons category
Snow
Commons gallery
Snow
Unicode character
melting point
0
Sources (6)

via Wikidata · CC0

~50 min read

Article

41 sections
Contents
  • Precipitation
  • Cloud formation
  • Low-pressure areas
  • Fronts
  • Lake and ocean effects
  • Mountain effects
  • Cloud physics
  • Classification of snowflakes
  • Accumulation
  • Event
  • Distribution
  • Records
  • Metamorphism
  • Seasonal
  • Firn
  • Movement
  • Drifting
  • Avalanche
  • Melting
  • Glaciers
  • Science
  • Measurement and classification
  • Satellite data
  • Models
  • Effects on civilization
  • Transportation
  • Highway
  • Aviation
  • Rail
  • Construction
  • Agriculture
  • Structures
  • Roofs
  • Utility lines
  • Sports and recreation
  • Warfare
  • Effects on plants and animals
  • Outside of Earth
  • See also
  • References
  • External links

Snow consists of individual ice crystals that grow while suspended in the atmosphere—usually within clouds—and then fall, accumulating on the ground where they undergo further changes. It consists of frozen crystalline water throughout its life cycle, starting when, under suitable conditions, the ice crystals form in the atmosphere, increase to millimeter size, precipitate and accumulate on surfaces, then metamorphose in place, and ultimately melt, slide, or sublimate away.

Snowstorms organize and develop by feeding on sources of atmospheric moisture and cold air. Snowflakes nucleate around particles in the atmosphere by attracting supercooled water droplets, which freeze in hexagonal-shaped crystals. Snowflakes take on a variety of shapes, basic among these are platelets, needles, columns, and rime. As snow accumulates into a snowpack, it may blow into drifts. Over time, accumulated snow metamorphoses, by sintering, sublimation, and freeze-thaw. Where the climate is cold enough for year-to-year accumulation, a glacier may form. Otherwise, snow typically melts seasonally, causing runoff into streams and rivers and recharging groundwater.

Gallery (52)

Available in 199 languages

Show 180 more

via Wikidata sitelinks · CC0

Connections

Categories