Small roundish masses of ice precipitated from the clouds, where they are formed by the congelation of vapor.
The separate masses or grains are called hailstones.
To pour down particles of ice, or frozen vapors.
To pour forcibly down, as hail.
To call loudly to, or after; to accost; to salute; to address.
To name; to designate; to call.
To declare, by hailing, the port from which a vessel sails or where she is registered; hence, to sail; to come; used with from; as, the steamer hails from New York.
To report as one's home or the place from whence one comes; to come; with from.
An exclamation of respectful or reverent salutation, or, occasionally, of familiar greeting.
Precipitation that originates in convective clouds, such as cumulonimbus, in the form of balls or irregular pieces of ice, which comes in different shapes and sizes Hail is considered to have a diameter of 5 millimeter or more; smaller bits of ice are classified as ice pellets, snow pellets, or graupel Individual lumps are called hailstones It is reported as 'GR' in an observation and on the METAR Small hail and/or snow pellets is reported as 'GS' in an observation and on the METAR.
Precipitation that originates in convective clouds, such as cumulonimbus, in the form of balls or irregular pieces of ice, which comes in different shapes and sizes Hail is considered to have a diameter of 5 millimeter or more; smaller bits of ice are classified as ice pellets, snow pellets, or graupel Individual lumps are caled hailstones.
Precipitation in the form of balls or irregular lumps of ice.
Falling ice in roughly round shapes at least 0 2 of an inch in diameter Hail comes from thunderstorms and is larger than sleet Hailstones form when upward moving air -- updrafts -- in a thunderstorm keep pieces of graupel from falling Drops of supercooled water hit and freeze to the graupel, causing it to grow When the balls of ice become too heavy for the updrafts to continue supporting them, they fall as hailstones Sleet, in contrast, consists of raindrops that freeze on the way down.
Hail is a destructive form of precipitation that is 5 to 190 millimeters in diameter The large downdrafts in mature thunderstorm clouds provide the mechanism for hail formation Hailstones normally have concentric shells of ice alternating between those with a milky appearance and those that are clear The milky white shells, containing bubbles and partially melted snowflakes, correspond to a period of rapid freezing, while the clear shells develop as the liquid water freezes much more slowly.
Precipitation in the form of balls or clumps of ice produced by thunderstorms Severe storms with intense updrafts are most likely to produce large hail.
Precipitation in the form of transparent or partially opaque balls or irregular lumps of concentric ice Hail is normally defined as having a diameter of 5 millimeters or more and is produced by thunderstorms.
Precipitation in the form of balls or irregular lumps of ice Tall cumulonimbus clouds are much warmer at the bottom than at the top This causes tremendous pressure differences and strong rising air currents, which suck warm water droplets from the bottom of the clouds to the top There, they freeze If the currents are strong enough, a hailstone will fall and rise many times, causing several layers of ice to build up until the hailstone is heavy enough to fall from the cloud.
Precipitation in the form of balls or irregular lumps of ice produced by liquid precipitation freezing and being coated by layers of ice as it is lifted and cooled in strong updrafts of thunderstorms.
Hail is observed precipitation in the form of small balls or pieces of ice , falling either separately or agglomerated into irregular lumps Hail falls during heavy thunderstorms.
Precipitation of small balls or other pieces of ice falling separately or frozen together in irregular lumps.
Sparse hailstones of small size, often mixed with rain Moderate:.
Wish of health; a salutation; a loud call.
Enthusiastic greeting precipitation of ice pellets when there are strong rising air currents greet enthusiastically or joyfully call for; 'hail a cab' be a native of; 'She hails from Kalamazoo' precipitate as small ice particles; 'It hailed for an hour'.
Precipitation of ice pellets when there are strong rising air currents.
Praise vociferously; 'The critics hailed the young pianist as a new Rubinstein'.
Be a native of; 'She hails from Kalamazoo'.
Call for; 'hail a cab'.
Greet enthusiastically or joyfully.
Precipitate as small ice particles; 'It hailed for an hour'.
Pieces of ice that fall from thunderstorms Hail often is composed of concentric rings of ice that form as the particle moves through 'wet' and 'dry' areas of the thunderstorm.
Precipitation which forms into balls or lumps of ice over 0 2 inch in diameter Hail is formed by alternate freezing and melting as it is carried up and down by turbulent air currents within a cloud.
Showery precipitation in the form of irregular pellets or balls of ice more than 5 mm in diameter, falling from a cumulonimbus cloud.
Precipitation composed of balls or irregular lumps of ice with diameters between 5 and 50 mm.
Precipitation composed of chunks of ice that form atop cumulonimbus clouds and fall as soon as they become too heavy for the cloud updrafts to hold.
Precipitation in the form of balls or lumps usually consisting of concentric layers of ice A thunderstorm is classified as severe when it produces hail 3/4 of an inch or larger in diameter The following table shows hail size estimates:.
İs precipitation composed of lumps of ice Hail is produced when large frozen raindrops or other particles in cumulonimbus clouds, grow by accumulating supercooled liquid droplets Violent updrafts in the cloud carry the particles up through the freezing all; allowing the frozen core to accumulate more ice when the piece of hail becomes too heavy to be carried by rising air currents, it falls to the ground.
Millimetric or larger precipitation particle of ice, formed by the accretion of ice crystals and rapidly freezing supercooled water droplets.
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