Graupel: The Snowflake That Isn’t Quite Snow or Hail
Graupel: The Snowflake That Isn’t Quite Snow or Hail
US · Published Nov 7, 2025
Graupel is formed when snowflakes collect supercooled water droplets that freeze on contact, creating soft, snow-like pellets.
Often mistaken for snow or hail, graupel is softer than hail and denser than snow, typically signaling unstable air and potential winter storms.
Graupel formation removes supercooled water from clouds, influencing precipitation patterns and contributing to faster accumulation on the ground.
Graupel: a unique precipitation, mistaken for snow
Graupel is a fascinating form of precipitation that often gets mistaken for snow or hail, but it's distinctly its own phenomenon. These soft, snow-like pellets form when snowflakes encounter supercooled water droplets in the atmosphere. These droplets, still in liquid form despite being below freezing, instantly freeze upon contact with the snowflake, creating a coating of ice. This process repeats as the snowflake tumbles through the air, accumulating layers of ice and forming a small, rounded pellet.
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