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- Hail abstract "Hail is a form of solid precipitation. It is distinct from sleet, though the two are often confused for one another It consists of balls or irregular lumps of ice, each of which is called a hailstone. Sleet falls generally in cold weather while hail growth is greatly inhibited at cold temperatures. Unlike graupel, which is made of rime, and ice pellets, which are smaller and translucent, hailstones consist mostly of water ice and measure between 5 millimetres (0.2 in) and 15 centimetres (6 in) in diameter. The METAR reporting code for hail 5 mm (0.20 in) or greater is GR, while smaller hailstones and graupel are coded GS. Hail is possible within most thunderstorms as it is produced by cumulonimbi, and within 2 nautical miles (3.7 km) of the parent storm. Hail formation requires environments of strong, upward motion of air with the parent thunderstorm (similar to tornadoes) and lowered heights of the freezing level. In the mid-latitudes, hail forms near the interiors of continents, while in the tropics, it tends to be confined to high elevations.There are methods available to detect hail-producing thunderstorms using weather satellites and weather radar imagery. Hailstones generally fall at higher speeds as they grow in size, though complicating factors such as melting, friction with air, wind, and interaction with rain and other hailstones can slow their descent through Earth's atmosphere. Severe weather warnings are issued for hail when the stones reach a damaging size, as it can cause serious damage to human-made structures and, most commonly, farmers' crops.".
- Hail thumbnail Granizo.jpg?width=300.
- Hail wikiPageExternalLink hail.
- Hail wikiPageExternalLink www.hailtrends.com.
- Hail wikiPageExternalLink Hail.html.
- Hail wikiPageID "14458".
- Hail wikiPageRevisionID "606261129".
- Hail hasPhotoCollection Hail.
- Hail subject Category:Precipitation.
- Hail subject Category:Snow_or_ice_weather_phenomena.
- Hail subject Category:Storm.
- Hail subject Category:Weather_hazards.
- Hail comment "Hail is a form of solid precipitation. It is distinct from sleet, though the two are often confused for one another It consists of balls or irregular lumps of ice, each of which is called a hailstone. Sleet falls generally in cold weather while hail growth is greatly inhibited at cold temperatures.".
- Hail label "Grad".
- Hail label "Grandine".
- Hail label "Granizo".
- Hail label "Granizo".
- Hail label "Grêle".
- Hail label "Hagel (neerslag)".
- Hail label "Hagel".
- Hail label "Hail".
- Hail label "Град".
- Hail label "برد (هطول)".
- Hail label "冰雹".
- Hail label "雹".
- Hail sameAs Kroupy_(meteorologie).
- Hail sameAs Hagel.
- Hail sameAs Χαλάζι.
- Hail sameAs Granizo.
- Hail sameAs Txingor.
- Hail sameAs Grêle.
- Hail sameAs Hujan_es.
- Hail sameAs Grandine.
- Hail sameAs 雹.
- Hail sameAs 우박.
- Hail sameAs Hagel_(neerslag).
- Hail sameAs Grad.
- Hail sameAs Granizo.
- Hail sameAs m.03rby.
- Hail sameAs Q37602.
- Hail sameAs Q37602.
- Hail wasDerivedFrom Hail?oldid=606261129.
- Hail depiction Granizo.jpg.
- Hail isPrimaryTopicOf Hail.