hajlítotok

Hajlítotok, also known as hailstones, are a form of precipitation consisting of balls or irregular lumps of ice. They are formed when supercooled water droplets freeze onto a condensation nucleus, such as a dust particle or ice crystal, within a thunderstorm cloud. As the hailstone falls through the cloud, it can accumulate more layers of ice, growing larger and larger. The size of hailstones can vary greatly, ranging from small pellets to large, golf ball-sized stones.

Hail typically falls during severe thunderstorms, which are characterized by strong updrafts and downdrafts. These storms can produce hailstones of various sizes, with larger hailstones often indicating more intense storms. Hail can cause significant damage to crops, vehicles, and buildings, and can also pose a risk to human safety due to its size and weight.

The study of hail, known as hail science, involves understanding the processes that lead to its formation and the factors that influence its size and distribution. Researchers use various tools, including radar and weather satellites, to monitor and predict hailstorms. By improving our understanding of hail, scientists can help communities better prepare for and mitigate the impacts of these severe weather events.