Hail
✨ The Sky's Ice Cubes
Hail is a form of solid precipitation made up of balls or irregular lumps of ice called hailstones. It forms inside powerful thunderstorm clouds, known as cumulonimbus clouds, where strong upward air currents repeatedly lift water droplets high into very cold parts of the cloud. There, the droplets freeze and grow as new layers of supercooled water freeze around them.
This cycle may happen several times before the hailstones become too heavy for the rising air to support. They then fall to the ground, sometimes together with heavy rain, strong winds and lightning. Hailstones vary greatly in size, from only a few millimeters across to several centimeters during the most intense storms.
Unlike snow, which develops as ice crystals, hail forms through repeated freezing inside thunderstorm clouds. It can occur in many parts of the world, especially during warm seasons when the atmosphere is unstable enough to produce powerful storms. Large hailstones may damage crops, roofs, windows and vehicles, while also posing a risk to people and animals caught outdoors.
Weather radars help meteorologists detect hail-producing storms and issue warnings before they reach populated areas. Although hailstorms usually last only a short time, they can cause significant local damage. Studying how hail forms also helps scientists better understand severe thunderstorms and improve weather forecasting.