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How does hail form?
Quick answer
Hail forms in thunderstorms when updrafts lift raindrops into freezing air, turning them into ice. These ice pellets grow by collecting supercooled water, which freezes in layers. Once too heavy for the updraft, they fall as hailstones, ranging from pea-sized to softball-sized.
Hail forms when strong updrafts in thunderstorms carry raindrops high into freezing air, where they freeze into ice pellets. These pellets grow larger as they collide with supercooled water droplets, eventually falling when they become too heavy for the updraft to support.
Step by step
- A strong thunderstorm updraft carries water droplets upward into air colder than 0°C.
- The droplets freeze into small ice particles, which serve as the cores of hailstones.
- Supercooled water droplets in the cloud collide with these ice cores and freeze onto them.
- The updraft keeps the growing hailstones aloft, allowing multiple layers of ice to accumulate.
- When the hailstone becomes too heavy for the updraft, it falls toward the ground.
- During its fall, the hailstone may partially melt if it passes through warm air near the surface.
Key things to understand
- Hailstones begin as small ice particles in the cold upper regions of cumulonimbus clouds.
- Supercooled water droplets, which remain liquid below 0°C, freeze onto these particles when they collide.
- The stronger the updraft, the longer the hailstone stays aloft and the more layers of ice it accumulates.
- Each trip through the cloud adds a new layer, creating concentric rings visible when the hailstone is cut open.
- When the hailstone becomes too heavy for the updraft, it falls to the ground, melting partially if the air below is warm.
Labelled diagram
- Updraft
Strong rising air carries water droplets upward into freezing temperatures.
- Freezing Level
Altitude where air temperature drops below 0°C, causing droplets to freeze.
- Ice Core
Initial frozen droplet that becomes the center of a hailstone.
- Supercooled Water
Liquid water below 0°C that freezes onto the ice core upon contact.
- Layered Growth
Repeated collisions add concentric ice layers as the hailstone circulates.
- Fall
Hailstone becomes too heavy for updraft and falls to the ground.
Real-world examples
- In the United States, the Great Plains region experiences frequent hailstorms, often called 'Hail Alley'.
- A 2018 hailstorm in Colorado produced hailstones larger than baseballs, causing significant damage.
- In India, hailstorms in the northern plains during pre-monsoon season can destroy standing crops.
- The world's largest recorded hailstone fell in Vivian, South Dakota, in 2010, measuring 8 inches in diameter.
Common mistake
✗ Myth: Hail forms only in winter because it is ice.
✓ Fact: Hail actually forms most often in summer, when thunderstorms are frequent and strong updrafts can carry water high into freezing air. The ice then falls through warm air, but large hailstones may not melt completely before reaching the ground.
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Part of the guide: Water & Weather Phenomena →

