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  == Definition ==
  
  == Definition ==


  
  Any thunderstorm which produces hail that reaches the ground is known as a hailstorm.<ref>{{cite web|url=http://amsglossary.allenpress.com/glossary/search?p=1&query=Hailstorm|title=Hailstorm|author=Glossary of Meteorology|year=2009|accessdate=2009-08-29|publisher=[[American Meteorological Society]]}}</ref>  Hail has a diameter of {{convert|5|mm|in}} or more.<ref name="gloss">{{cite web|url=http://amsglossary.allenpress.com/glossary/search?id=hail1|title=Hail|year=2009|accessdate=2009-07-15|author=Glossary of Meteorology|publisher=[[American Meteorological Society]]}}</ref> Hailstones can grow to {{convert|15|cm|in|0}} and weigh more than {{convert|0.5|kg|lb|1}}.<ref>{{cite web|url=http://www.photolib.noaa.gov/htmls/nssl0001.htm|title=Aggregate hailstone|author=National Severe Storms Laboratory|publisher=[[National Oceanic and Atmospheric Administration]]|date=2007-04-23|accessdate=2009-07-15}}</ref>
  
  Any thunderstorm these motherfuckers which produces hail that reaches the ground is known as a hailstorm.<ref>{{cite web|url=http://amsglossary.allenpress.com/glossary/search?p=1&query=Hailstorm|title=Hailstorm|author=Glossary of Meteorology|year=2009|accessdate=2009-08-29|publisher=[[American Meteorological Society]]}}</ref>  Hail has a diameter of {{convert|5|mm|in}} or more.<ref name="gloss">{{cite web|url=http://amsglossary.allenpress.com/glossary/search?id=hail1|title=Hail|year=2009|accessdate=2009-07-15|author=Glossary of Meteorology|publisher=[[American Meteorological Society]]}}</ref> Hailstones can grow to {{convert|15|cm|in|0}} and weigh more than {{convert|0.5|kg|lb|1}}.<ref>{{cite web|url=http://www.photolib.noaa.gov/htmls/nssl0001.htm|title=Aggregate hailstone|author=National Severe Storms Laboratory|publisher=[[National Oceanic and Atmospheric Administration]]|date=2007-04-23|accessdate=2009-07-15}}</ref>


  
  

  
  



  
  Unlike ice pellets, hailstones are layered and can be irregular and clumped together.  Hail is composed of transparent ice or alternating layers of transparent and translucent ice at least {{convert|1|mm|in}} thick, which are deposited upon the hailstone as it travels through the cloud, suspended aloft by air with strong upward motion until its weight overcomes the [[vertical draft|updraft]] and falls to the ground. Although the diameter of hail is varied, in the United States, the average observation of damaging hail is between 2.5&nbsp;cm (1&nbsp;in) and [[golf ball]]-sized (1.75&nbsp;in).<ref>{{cite web|url=http://www.spc.noaa.gov/publications/jewell/hailslsc.pdf|title=P9.5 Evaluation of an Alberta Hail Growth Model Using Severe Hail Proximity Soundings in the United States|author=Ryan Jewell and Julian Brimelow|date=2004-08-17|accessdate=2009-07-15}}</ref>
  
  Unlike ice pellets, hailstones are layered and can be irregular and clumped together.  Hail is composed of transparent ice or alternating layers of transparent and translucent ice at least {{convert|1|mm|in}} thick, which are deposited upon the hailstone as it travels through the cloud, suspended aloft by air with strong upward motion until its weight overcomes the [[vertical draft|updraft]] and falls to the ground. Although the diameter of hail is varied, in the United States, the average observation of damaging hail is between 2.5&nbsp;cm (1&nbsp;in) and [[golf ball]]-sized (1.75&nbsp;in).<ref>{{cite web|url=http://www.spc.noaa.gov/publications/jewell/hailslsc.pdf|title=P9.5 Evaluation of an Alberta Hail Growth Model Using Severe Hail Proximity Soundings in the United States|author=Ryan Jewell and Julian Brimelow|date=2004-08-17|accessdate=2009-07-15}}</ref>
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 == Definition ==
-Any thunderstorm which produces hail that reaches the ground is known as a hailstorm.<ref>{{cite web|url=http://amsglossary.allenpress.com/glossary/search?p=1&query=Hailstorm|title=Hailstorm|author=Glossary of Meteorology|year=2009|accessdate=2009-08-29|publisher=[[American Meteorological Society]]}}</ref>  Hail has a diameter of {{convert|5|mm|in}} or more.<ref name="gloss">{{cite web|url=http://amsglossary.allenpress.com/glossary/search?id=hail1|title=Hail|year=2009|accessdate=2009-07-15|author=Glossary of Meteorology|publisher=[[American Meteorological Society]]}}</ref> Hailstones can grow to {{convert|15|cm|in|0}} and weigh more than {{convert|0.5|kg|lb|1}}.<ref>{{cite web|url=http://www.photolib.noaa.gov/htmls/nssl0001.htm|title=Aggregate hailstone|author=National Severe Storms Laboratory|publisher=[[National Oceanic and Atmospheric Administration]]|date=2007-04-23|accessdate=2009-07-15}}</ref>
+Any thunderstorm these motherfuckers which produces hail that reaches the ground is known as a hailstorm.<ref>{{cite web|url=http://amsglossary.allenpress.com/glossary/search?p=1&query=Hailstorm|title=Hailstorm|author=Glossary of Meteorology|year=2009|accessdate=2009-08-29|publisher=[[American Meteorological Society]]}}</ref>  Hail has a diameter of {{convert|5|mm|in}} or more.<ref name="gloss">{{cite web|url=http://amsglossary.allenpress.com/glossary/search?id=hail1|title=Hail|year=2009|accessdate=2009-07-15|author=Glossary of Meteorology|publisher=[[American Meteorological Society]]}}</ref> Hailstones can grow to {{convert|15|cm|in|0}} and weigh more than {{convert|0.5|kg|lb|1}}.<ref>{{cite web|url=http://www.photolib.noaa.gov/htmls/nssl0001.htm|title=Aggregate hailstone|author=National Severe Storms Laboratory|publisher=[[National Oceanic and Atmospheric Administration]]|date=2007-04-23|accessdate=2009-07-15}}</ref>
 Unlike ice pellets, hailstones are layered and can be irregular and clumped together.  Hail is composed of transparent ice or alternating layers of transparent and translucent ice at least {{convert|1|mm|in}} thick, which are deposited upon the hailstone as it travels through the cloud, suspended aloft by air with strong upward motion until its weight overcomes the [[vertical draft|updraft]] and falls to the ground. Although the diameter of hail is varied, in the United States, the average observation of damaging hail is between 2.5&nbsp;cm (1&nbsp;in) and [[golf ball]]-sized (1.75&nbsp;in).<ref>{{cite web|url=http://www.spc.noaa.gov/publications/jewell/hailslsc.pdf|title=P9.5 Evaluation of an Alberta Hail Growth Model Using Severe Hail Proximity Soundings in the United States|author=Ryan Jewell and Julian Brimelow|date=2004-08-17|accessdate=2009-07-15}}</ref>
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