Hail is a form of solid precipitation. source
Hail is a form of solid precipitation.
Hail is distinct from ice pellets (sleet), though the two are often confused. source
Hail is distinct from ice pellets (sleet), though the two are often confused.
Hail consists of balls or irregular lumps of ice, each of which is called a hailstone. source
Hail consists of balls or irregular lumps of ice, each of which is called a hailstone.
Ice pellets (sleet) falls generally in cold weather while hail growth is greatly inhibited during cold surface temperatures. source
Ice pellets (sleet) falls generally in cold weather while hail growth is greatly inhibited during cold surface temperatures.
Hail is possible within most thunderstorms as it is produced by cumulonimbus,and within 2 nautical miles (3.7 km) of the parent storm. source
Hail is possible within most thunderstorms as it is produced by cumulonimbus,and within 2 nautical miles (3.7 km) of the parent storm.
In the mid-latitudes, hail forms near the interiors of continents, while in the tropics, it tends to be confined to high elevations. source
In the mid-latitudes, hail forms near the interiors of continents, while in the tropics, it tends to be confined to high elevations.
There are methods available to detect hail-producing thunderstorms using weather satellites and weather radar imagery. source
There are methods available to detect hail-producing thunderstorms using weather satellites and weather radar imagery.
Hailstones generally fall at higher speeds as they grow in size, though complicating factors such as melting, friction with air, wind, source
Hailstones generally fall at higher speeds as they grow in size, though complicating factors such as melting, friction with air, wind,
Hail occurs most frequently within continental interiors at mid-latitudes and is less common in the tropics. source
Hail occurs most frequently within continental interiors at mid-latitudes and is less common in the tropics.
Hail begins as water droplets. source
Hail begins as water droplets.
Hail is most common within continental interiors of the mid-latitudes. source
Hail is most common within continental interiors of the mid-latitudes.
The size of hailstones is best determined by measuring their diameter with a ruler. source
The size of hailstones is best determined by measuring their diameter with a ruler.
Hail can cause serious damage, notably to automobiles, aircraft, skylights, glass-roofed structures, livestock, and most commonly, farmers' crops. source
Hail can cause serious damage, notably to automobiles, aircraft, skylights, glass-roofed structures, livestock, and most commonly, farmers' crops.
Hail damage to roofs often goes unnoticed until further structural damage is seen, such as leaks or cracks. source
Hail damage to roofs often goes unnoticed until further structural damage is seen, such as leaks or cracks.
Hail is one of the most significant thunderstorm hazards to aircraft source
Hail is one of the most significant thunderstorm hazards to aircraft
When hailstones exceed 0.5 inches (13 mm) in diameter, planes can be seriously damaged within seconds. source
When hailstones exceed 0.5 inches (13 mm) in diameter, planes can be seriously damaged within seconds.
Massive hailstones have been known to cause concussions or fatal head trauma source
Massive hailstones have been known to cause concussions or fatal head trauma
