Hail or Sleet, How to Tell the Difference

There are two easy facts to differentiate between hail and sleet: time of year and size. Using these essentials, it is easy to identify what kind of frozen precipitation is falling.

This picture of a record-sized hail ball is courtesy of NOAA.

Hail:

Hail occurs during severe weather. Hail is the formed when an object, including dust or particles in the air, collides with supercooled water. As the water freezes around the object, it begins to form an ice pellet. To understand this, you have to remember that warm air rises and cool air sinks (the same as heating or cooling in your house) this is because colder air is more dense than warmer air. Normally, warm air is very buoyant in the clouds that are associated with thunderstorms. This buoyancy causes these clouds to rise higher into the atmosphere past the freezing level.

The length of time the ice pellet stays in the cloud is a representation of how large it will be when it falls to the ground. How does it increase in size? Inside the cloud, there are a series of updrafts. The pellet will continue to be tossed up and down, adding layers of ice, until it becomes too heavy for the updraft. When the hail becomes too heavy, it then falls to the ground. Usually accompanying severe thunderstorms, hail can be a variety of sizes, many times correlating with the intensity of the thunderstorms. Certain hail can get as large as golf balls, softballs or even larger! The largest hailstone ever found was in Vivian, S.D., it weighed 1.9 pounds and measured 8 inches in diameter with an 18.5-inch circumference.

Sleet

Sleet occurs during winter weather and is a type of winter precipitation. All precipitation falls out of a cloud as snow. In certain instances, in the winter, the snowflake will go through a warmer layer and begin to melt. As it continues to fall, it will then proceed through a colder layer and freeze into an ice pellet or ball, very similar to hail. Unlike hail, the pellet only "falls" once and is generally very tiny in size.

More Weather Glossary

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    Squall lines occur when intense thunderstorms organize into a solid line. Along the leading edge of the storms, winds can be quite destructive, sometimes topping 60, 70 and even 80 mph.

  • Why Is the Radar Sometimes Wrong?

    A weather radar follows some of the same principles at a flashlight. While a flashlight uses rays of light to detect objects in the dark, radars detect objects in the atmosphere using pulses of energy.

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This Day In Weather History

Chicago, IL (1992)
32 degrees, latest 32 or lower on record.

Iowa City, IA (1859)
Waterspout; 8 killed, one child was taken up, carried 500 yards and thrown in a slough but survived.

Philadelphia, PA (1991)
96 degrees -- a record sixth 90-degree reading for the month. (The month ended with twelve 90-degree days.)