snow

—snowless, adj. —snowlike, adj.

/snoh/, n.

1. Meteorol. a precipitation in the form of ice crystals, mainly of intricately branched, hexagonal form and often agglomerated into snowflakes, formed directly from the freezing of the water vapor in the air. Cf. ice crystals, snow grains, snow pellets.

2. these flakes as forming a layer on the ground or other surface.

3. the fall of these flakes or a storm during which these flakes fall.

4. something resembling a layer of these flakes in whiteness, softness, or the like: the snow of fresh linen.

5. Literary.

a. white blossoms.

b. the white color of snow.

6. Slang. cocaine or heroin.

7. white spots or bands on a television screen caused by a weak signal. Cf. hash¹ (def. 5).

v.i.

8. to send down snow; fall as snow.

9. to descend like snow.

v.t.

10. to let fall as or like snow.

11. Slang.

a. to make an overwhelming impression on: The view really snowed them.

b. to persuade or deceive: She was snowed into believing everything.

12. snow under,

a. to cover with or bury in snow.

b. to overwhelm with a larger amount of something than can be conveniently dealt with.

c. to defeat overwhelmingly.

[bef. 900; (n.) ME; OE snaw; c. D sneeuw, G Schnee, ON snaer, Goth snaiws, L nix (gen. nivis), Gk níps (acc. nípha), OCS snegu; (v.) ME snowen, deriv. of the n.; r. ME snewen, OE sniwan; c. OHG sniwan (G schneien), MLG, MD snien]

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I

Solid form of water that crystallizes in the atmosphere and falls to the Earth, covering about 23% of the Earth's surface either permanently or temporarily.

Snowflakes are formed by crystals of ice that generally have a hexagonal pattern. Snow cover has a significant effect on climate and on plant, animal, and human life. By increasing the reflection of solar radiation and interfering with the conduction of heat from the ground, it induces a cold climate. The low heat conduction protects small plants from the effects of the lowest winter temperatures; on the other hand, late disappearance of snow in the spring delays the growth of plants.

II

(as used in expressions)

snow leopard

Snow Charles Percy

Baron Snow of the City of Leicester

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▪ weather

      the solid form of water that crystallizes in the atmosphere and, falling to the Earth, covers, permanently or temporarily, about 23 percent of the Earth's surface.

      A brief treatment of snow follows. For full treatment, see climate: Snow and sleet (climate).

      Snow falls at sea level poleward of latitude 35° N and 35° S, though on the west coast of continents it generally falls only at higher latitudes. Close to the equator, snowfall occurs exclusively in mountain regions—at elevations of about 4,900 m (16,000 feet) or higher.

      Snow cover has a significant effect on climate and on plant, animal, and human life. By increasing the reflection of solar radiation and interfering with the conduction of heat from the ground, it induces a cold climate. The low heat conduction protects small plants from the effects of the lowest winter temperatures; on the other hand, the late disappearance of snow in the spring delays the growth of plants. When snow melts in the spring, the resulting runoff feeds rivers and supplies water for irrigation and other human enterprises. Heavy snowfalls can severely hinder transporation in variable moderate climates but provides a firm surface for travel in remote Arctic, Antarctic, and mountainous areas, using traditional dogsleds or snowshoes or modern snowmobiles.

 Snowflakes are formed by crystals of ice that generally have a hexagonal pattern, often beautifully intricate (see video—>). The size and shape of the crystals depend mainly on the temperature and the amount of water vapour available as they develop. At temperatures above about -40° C (-40° F), ice crystals form around minute particles of dust or chemical substances that float in the air; at lower temperatures, crystals form directly from water vapour. If the air is humid, the crystals tend to grow rapidly, develop branches, and clump together to form snowflakes. In colder and drier air, the particles remain small and compact. Frozen precipitation has been classified into seven forms of snow crystals and three types of particles—graupel (granular snow pellets, also called soft hail), sleet (partly frozen ice pellets), and hail (hard spheres of ice).

      The texture and density of fallen snow undergo constant change. Snow on the ground tends to become increasingly dense, and, where it survives spring and summer melting for years, it may turn into ice and form a glacier. On hillsides when temperature changes reduce the coherence of snow particles in the snow cover, gravity and viscosity may overcome friction, causing snow slides and avalanches.

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