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hail1

  (hāl) pronunciation
n.
  1. Precipitation in the form of spherical or irregular pellets of ice larger than 5 millimeters (0.2 inches) in diameter.
  2. Something that falls with the force and quantity of a shower of ice and hard snow: a hail of pebbles; a hail of criticism.

v., hailed, hail·ing, hails.

v.intr.
  1. To precipitate in pellets of ice and hard snow.
  2. To fall like hailstones: Condemnations hailed down on them.
v.tr.

To pour (something) down or forth: They hailed insults at me.

[Middle English, from Old English hægel, hagol.]


 
 

Precipitation composed of chunks or lumps of ice formed in strong updrafts in cumulonimbus clouds. Individual lumps are called hailstones. Most hailstones are spherical or oblong, some are conical, and some are bumpy and irregular. Diameters range from 0.2 to 6 in. (5 to 150mm) or more. That is, the largest stones are grapefruit or softball size, and the smallest are pea size.

Very often hailstones are observed to be made of alternating rings of clear and white ice (see illustration). These rings indicate the growth processes of the hail. The milky or white portion of the growth occurs when small cloud droplets are collected by the hailstone and freeze almost instantaneously, trapping bubbles of air between the droplets and creating a milky appearance. The clear portion is formed when many droplets arecollected so rapidly that a film of water spreads over the stone and freezes gradually, givingtime for any trapped air bubbles to escape from the liquid.

Cross section of a large hailstone showing the structure of alternating rings of clear and white ice. (<i>Alberta Research Council, Edmonton</i>)
Cross section of a large hailstone showing the structure of alternating rings of clear and white ice. (Alberta Research Council, Edmonton)

The most favorable conditions for hail formation occur in the mountainous, high plains regions of the world. Hailstorms normally have relatively high, cool cloud bases and very strong updrafts within the clouds to carry the hailstones into the cooler regions of the cloud, where maximum growth occurs. Both small ice particles and supercooled liquid water (liquid water at temperatures below 32°F or 0°C) are needed for the ice particles to grow into hailstones. See also Cloud physics; Precipitation (meteorology).


 
Thesaurus: hail1

noun

    A concentrated outpouring, as of missiles, words, or blows: barrage, bombardment, burst, cannonade, fusillade, salvo, shower, storm, volley. See attack/defend.

 
Antonyms: hail

v

Definition: rain down on
Antonyms: dribble, drip


 

Precipitation of balls or pieces of ice with a diameter of 0.2 – 4 in. (5 mm – 10 cm). Small hail (also called sleet, or ice pellets) has a diameter of less than 0.2 in. Hail can be extremely destructive to buildings and crops; if it is large enough, it may be dangerous to animals. Hailstones 6 in. (15 cm) in diameter have fallen during storms in the U.S. Midwest. Hailstorms are most common in the middle latitudes and usually last around 15 minutes. They ordinarily occur in middle to late afternoon and may accompany thunderstorms.

For more information on hail, visit Britannica.com.

 
precipitation in the form of pellets composed of ice or of ice and snow, occurring at any time of the year, usually during the passage of a cold front or during a thunderstorm. Small hailstones have a soft center and a single outer coat of ice. They are formed when the surfaces of snow clumps melt and refreeze or become coated with water droplets that subsequently freeze. Large hailstones usually have alternate hard and soft layers. There are various explanations of how these large stones form and grow. Some believe that they form in clouds when supercooled raindrops (i.e., drops chilled below the freezing temperature without solidifying) freeze on dust particles or snowflakes. These tiny hailstones are then blown repeatedly up and down by the winds in a cloud. Each time they are blown downward to a region whose temperature is above freezing, the stones collect more moisture, and each time they are blown upward to a region below freezing, the moisture solidifies into ice, and some snow may collect. The stones continue to grow, adding layer after layer, until they are too heavy to be supported by the winds and fall to the ground. In another explanation, it is suggested that hailstones continuously descend, gaining layers by passing through regions of the air that contain different amounts of water. Hailstones are spherical or irregularly spherical and usually vary in diameter up to 1/2 in. (1.3 cm); in rare cases hailstones having diameters up to 5 in. (12.7 cm) have been observed. Hail causes much damage and injury to crops, livestock, property, and airplanes. See sleet.


 

Pellets of ice that form when updrafts in thunderstorms carry raindrops to high altitudes, where the water freezes and then falls back to Earth. Hailstones as large as baseballs have been recorded. Hail can damage crops and property.

 
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Hail is a form of precipitation which consists of balls or irregular lumps of ice (hailstones). Hailstones on Earth usually consist mostly of water ice and measure between 5 and 50 millimetres in diameter, with the larger stones coming from severe thunderstorms.[1] Hail is always produced by cumulonimbi (thunderclouds), usually at the front of the storm system, and is composed of transparent ice or alternating layers of transparent and translucent ice at least 1 mm thick. Small hailstones are less than 5 mm in diameter, and are reported as SHGS. Unlike ice pellets, they are layered and can be irregular and clumped together.

Hail formation

A large hailstone, about 6 cm in diameter
Enlarge
A large hailstone, about 6 cm in diameter

Hail forms on condensation nuclei such as dust, insects, or ice crystals, when supercooled water freezes on contact. Hailstones are usually from the size of a pea to the size of a golfball. In clouds containing large numbers of supercooled water droplets, these ice nuclei grow quickly at the expense of the liquid droplets because the saturation vapor pressure over ice is slightly less than the saturation vapor pressure over water. If the hailstones grow large enough, latent heat released by further freezing may melt the outer shell of the hailstone. The growth that follows, usually called wet growth, is more efficient because the liquid outer shell allows the stone to accrete other smaller hailstones in addition to supercooled droplets. These winds hold the rain and freeze it. As the process repeats, the hail grows increasingly larger. Once a hailstone becomes too heavy to be supported by the storm's updraft it falls out of the cloud. When a hailstone is cut in half, a series of concentric rings, like that of an onion, is revealed. These rings reveal the total number of times the hailstone had traveled to the top of the storm before falling to the ground.


Ideal conditions for hail formation

The largest hailstone ever measured, 17.8 cm (7.0 in) in diameter with a 47.6 cm (18.75 in) circumference.
Enlarge
The largest hailstone ever measured, 17.8 cm (7.0 in) in diameter with a 47.6 cm (18.75 in) circumference.

Hail forms in strong thunderstorm clouds, particularly those with intense updrafts, high liquid water content, great vertical extent, large water droplets, and where a good portion of the cloud layer is below freezing (0 °C (32 °F)). The growth rate is maximized at about -13 °C (9 °F), and becomes vanishingly small much below -30 °C (-22 °F) as supercooled water droplets become rare. For this reason, hail is most common in midlatitudes during early summer where surface temperatures are warm enough to promote the instability associated with strong thunderstorms, but the upper atmosphere is still cool enough to support ice. Accordingly, hail is actually less common in the tropics despite a much higher frequency of thunderstorms than in the midlatitudes because the atmosphere over the tropics tends to be warmer over a much greater depth.[citation needed] Also, entrainment of dry air into strong thunderstorms over continents can increase the frequency of hail by promoting evaporational cooling which lowers the freezing level of thunderstorm clouds giving hail a larger volume to grow in.

Hail is also much more common along mountain ranges because mountains force horizontal winds upwards (known as orographic lifting), thereby intensifying the updrafts within thunderstorms and making hail more likely. One of the most notorious regions for large hail is northern India and Bangladesh, which have reported more hail-related deaths than anywhere else in the world and also some of the largest hailstones ever measured. Mainland China is also notorious for killer hailstorms. Certain locations in North America (such as the area around Calgary, Alberta) have gained the nickname "Hailstorm Alley" among meteorologists for the frequency of hailstorms and their severity.[1]

Hail clouds often exhibit a characteristic green coloration.
Enlarge
Hail clouds often exhibit a characteristic green coloration.

Hailstones, while most commonly only a few millimetres in diameter, can sometimes grow to 15 centimetres and weigh more than half a kilogram (1.1 pounds)[2]. Pea or golfball-sized hailstones are not uncommon in severe storms. Hail can do serious damage, notably to automobiles, skylights, glass-roofed structures, and most commonly, farmers' crops. Rarely, massive hailstones have been known to cause concussions or fatal head trauma. Sometimes, hail-producing clouds are identifiable by their green colouration.[2][3]

Costly or deadly hailstorms

April 20, 2006 hailstorm on San Marcos, Texas
Enlarge
April 20, 2006 hailstorm on San Marcos, Texas

Also, a freak hailstorm hit Los Angeles County in December, 1967, blanketing the region much like a snowstorm. The storm also produced lightning, and one bolt struck an oil tank in Manhattan Beach, causing an explosion that covered much of the South Bay with the oil. The next hailstorm to hit the area was in 1979.

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See also

References

    • Rogers and Yau (1989). A Short Course in CLOUD PHYSICS. Massachusetts: Butterworth-Heinemann. ISBN 0-7506-3215-1. 

    External links

    Wikimedia Commons has media related to:

     
    Translations: Translations for: Hail

    Dansk (Danish)
    1.
    n. - hagl, byge, regn
    v. intr. - hagle
    v. tr. - lade det hagle med

    idioms:

    • a hail of    en byge af

    2.
    v. tr. - hilse, hilse velkommen, hylde, råbe an
    v. intr. - stamme fra, praje
    int. - hil!
    n. - hilsen, råben, prajning, ballade, spektakel

    idioms:

    • hail from    stamme fra, komme fra
    • Hail Mary    Ave Maria
    • within hail    indenfor hørevidde

    Nederlands (Dutch)
    begroeten, aanroepen, erkennen als, trouw bekennen, hagelen, doen neerkomen, groet, 'Heil..!', hagel, hagelsteen, hagelstorm

    Français (French)
    1.
    n. - grêle, (fig) grêle de
    v. intr. - grêler
    v. tr. - héler

    idioms:

    • a hail of    une grêle/une avalanche de

    2.
    v. tr. - saluer qn (comme étant), acclamer qn comme
    v. intr. - saluer qn (comme étant), acclamer qn comme
    int. - Salut (excl)
    n. - salut

    idioms:

    • hail from    venir de (sout), être de
    • Hail Mary    (Relig) Ave ou Ave Maria, "Je vous salue Marie"
    • within hail    à portée de la victoire, proche de la victoire

    Deutsch (German)
    1.
    n. - Hagel
    v. - hageln

    idioms:

    • a hail of    ein -hagel, -regen

    2.
    v. - zujubeln, anrufen
    int. - heil!, sei gegrüßt!
    n. - Zuruf, Gruß

    idioms:

    • hail from    kommen von
    • Hail Mary    Ave Maria
    • within hail    hörbar

    Ελληνική (Greek)
    v. - προσφωνώ, χαιρετίζω, χαιρετώ, καλωσορίζω, επικροτώ, ζητωκραυγάζω, καλώ, κράζω, φωνάζω, ρίχνει χαλάζι
    n. - προσφώνηση, χαιρετισμός, κλήση, κραυγή, (μετεωρ.) χαλάζι

    idioms:

    • a hail of    καταιγισμός
    • hail from    κατάγομαι από, προέρχομαι από
    • Hail Mary    (θρησκ.) Χαιρετισμός (της Θεοτόκου)
    • within hail    (καθομ.) δυο βήματα, (πολύ) κοντά

    Italiano (Italian)
    salutare, grandinare, grandine

    idioms:

    • a hail of    una gragnuola di
    • hail from    venire da
    • Hail Mary    Ave Maria
    • within hail    a portata di voce

    Português (Portuguese)
    v. - saudar, aclamar, granizar
    n. - aclamação (f), granizo (m)

    idioms:

    • a hail of    saudações de
    • hail from    natural de
    • Hail Mary    Ave (f) Maria (Rel.)
    • within hail    à distância da voz

    Русский (Russian)
    приветствие, провозглашать, окликать, приветствовать, сыпаться градом, град, оклик

    idioms:

    • a hail of    град (чего-либо)
    • hail from    быть родом из, быть приписанным к какому-либо порту
    • Hail Mary    католическая молитва Аве Мария
    • within hail    недалеко, в пределах слышимости

    Español (Spanish)
    1.
    n. - granizo, granizada, lluvia
    v. intr. - granizar, llover
    v. tr. - granizar, llover

    idioms:

    • a hail of    una lluvia de

    2.
    v. tr. - llamar, saludar, aclamar
    v. intr. - llamar, saludar, aclamar
    int. - Salve!
    n. - llamado, saludo, aclamación

    idioms:

    • hail from    ser de, proceder de, venir de
    • Hail Mary    Avemaría
    • within hail    estar al alcance de la voz

    Svenska (Swedish)
    v. - hagla, hälsa, kalla på
    n. - hagel, hälsning, (an)rop

    中文(简体) (Chinese (Simplified))
    1. 欢呼, 打招呼, 招呼, 来自, 招呼致意, 向...欢呼, 承认...为, 为...喝彩, 拥立

    idioms:

    • a hail of    一阵的...
    • hail from    来自
    • Hail Mary    万福马利亚
    • within hail    在附近

    2. 使像冰雹般落下, 下冰雹, 冰雹般落下, 雹, 一阵, 冰雹, 好啊, 欢迎

    中文(繁體) (Chinese (Traditional))
    1.
    v. tr. - 使像冰雹般落下
    v. intr. - 下冰雹, 冰雹般落下
    n. - 雹, 一陣, 冰雹
    int. - 好啊, 歡迎

    2.
    n. - 歡呼, 打招呼
    v. intr. - 招呼, 來自, 招呼致意
    v. tr. - 向...歡呼, 承認...為, 為...喝彩, 擁立

    idioms:

    • a hail of    一陣的...
    • hail from    來自
    • Hail Mary    萬福馬利亞
    • within hail    在附近

    한국어 (Korean)
    1.
    n. - 우박, 쏟아지는 것, 싸락눈
    v. intr. - 싸락눈이 내리다, 빗발치듯 퍼 붓다
    v. tr. - ~을 빗발치듯 퍼 붓다

    idioms:

    • a hail of    ~의 빗발

    2.
    v. tr. - ~에게 인사하다, 환호하여 맞이하다, ~이라고 부르다
    v. intr. - 큰소리를 지르다
    int. - 만세, 야, 반갑네
    n. - 큰 소리로 부름, 인사, 환영

    idioms:

    • hail from    ~에서 오다, ~의 출신이다

    日本語 (Japanese)
    n. - ひょう, あられ, 雨あられのような…, 呼びかけ, 歓呼
    v. - あられが降る, 歓呼して迎える, 呼んで迎える, 大声で呼ぶ

    idioms:

    • a hail of    雨あられの
    • hail from    出身である, …から来る
    • Hail Mary    天使祝詞
    • within hail    声の届く所に

    العربيه (Arabic)
    ‏(فعل) تمطر السماء بردا, ينهمر كالبرد, ينادي, يحيي, يرحب ب, يمطره بوابل من (الاسم) برد, وابل كالبرد, تحيه, ترحيب, هتاف, نداء‏

    עברית (Hebrew)
    n. - ‮ברד‬
    v. intr. - ‮ירד (ברד)‬
    v. tr. - ‮המטיר‬
    v. tr. - ‮הריע, קרא, בירך, עשה סימן כדי למשוך שימת-לב‬
    v. intr. - ‮היה (במקורו) ממקום מסוים‬
    n. - ‮מרחק המשפיע על אפשרות הברכה, ברכה, קריאת שלום‬
    int. - ‮קריאת ברכה‬


     
     

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    Dictionary. The American Heritage® Dictionary of the English Language, Fourth Edition Copyright © 2007, 2000 by Houghton Mifflin Company. Updated in 2007. Published by Houghton Mifflin Company. All rights reserved.  Read more
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    Science Dictionary. The New Dictionary of Cultural Literacy, Third Edition Edited by E.D. Hirsch, Jr., Joseph F. Kett, and James Trefil. Copyright © 2002 by Houghton Mifflin Company. Published by Houghton Mifflin. All rights reserved.  Read more
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