Large damaging hailstones primarily occur during summer due to the presence of significant moisture in thunderclouds, specifically cumulonimbus clouds. These clouds develop when hot, moist air is trapped beneath cold, dry air, creating the ideal conditions for thunderstorms. As the storm intensifies, rainwater rises to high altitudes where it freezes, forming hailstones. The size of these hailstones is determined by the strength of the updrafts within the storm, which can keep the hail aloft long enough for additional layers of ice to accumulate. Eventually, the hailstones become too heavy and fall to the ground, resulting in damaging hail events.