Actions

::Ice pellets

::concepts

Pellets::national    Weather::layer    Sleet::surface    Volume::sleet    Title::canada    Glossary::ground

{{#invoke:sidebar|sidebar | class = hlist | pretitle = Part of the nature series | title = Weather

| headingstyle = border-top:#ccc 1px solid; | heading1 = Calendar seasons | content1 =

| heading2 = Tropical seasons | content2 =

| heading3 = Storms | content3 =

| heading4 = Precipitation | content4 =

| heading5 = Topics | content5 =

| belowstyle = border-top:#ccc 1px solid; border-bottom:#ccc 1px solid; | below = Weather portal

}}

Ice pellets are a form of precipitation consisting of small, translucent balls of ice. Ice pellets are smaller than hailstones<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> which form in thunderstorms rather than in winter, and are different from graupel ("soft hail") which is made of frosty white rime, and from a mixture of rain and snow which is a slushy liquid or semisolid. Ice pellets often bounce when they hit the ground or other solid objects, and make a higher-pitched "tap" when striking objects like jackets, windshields, and dried leaves, compared to the dull splat of liquid raindrops. Pellets generally do not freeze into a solid mass unless mixed with freezing rain. The METAR code for ice pellets is PL (PE before November 1998<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>).


Ice pellets sections
Intro   Terminology    Formation    Effects    See also    References   

PREVIOUS: IntroNEXT: Terminology
<<>>