Dual Enrollment Physical Science Midterm Practice Test 2026 – The Complete All-in-One Guide for Exam Success!

Thunderstorms generate strong updrafts that lift water droplets high into parts of the cloud where temperatures are below freezing. There, droplets freeze and begin to form ice pellets. As the storm’s updrafts keep cycling these pellets through freezing layers and through supercooled droplets, they accumulate ice and grow into hailstones. When the updrafts are especially strong, hail can grow large before gravity pulls it down, making hail a hallmark precipitation type for thunderstorms, particularly severe ones, because it directly reflects how the storm lifts and freezes water.

Snow, sleet, and freezing rain involve different atmospheric temperature structures. Snow comes from ice crystals forming in cold clouds, not from the same convective updraft process that creates hail. Sleet forms when falling snow partially melts and then refreezes before reaching the ground, and freezing rain happens when rain falls through a shallow cold layer that freezes on contact with surfaces. While these can occur in some storm setups, they’re not the typical precipitation outcome produced by the vigorous updrafts of thunderstorms like hail is.