• 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.