The cumulonimbus cloud can produce destructive weather like thunderstorms, heavy rain, hailstorms, and even tornadoes. The world record hailstone fell in Kansas, USA weighing 1.7 lbs and 7.5 inches in diameter. Hailstones form inside the cumulonimbus cloud as water droplets are cycled between different temperature layers, freezing onto the hailstone and adding layers of ice. Powerful updrafts and downdrafts inside the cloud influence the size of the hailstone by cycling it between layers for longer periods of time. A large hailstorm in Sydney, Australia in 1999 caused extensive property damage but no deaths.

1. WEATHER LORE CUMULONIMBUS AND HAIL

2. The mechanisms at work inside a cumulonimbus cloud are very special indeed. It is this cloud, towering up to 12 km or more in height, that brings our most impressive and potentially destructive weather.

3. Thunderstorms, intense rainfall, squalls, hailstorms and even tornadoes commonly accompany this ‘danger’ cloud, particularly with a so-called ‘Supercell’.

4. Less obviously devastating than a tornado, hailstorms do immense damage, particularly in continental interiors such as the USA. Here the intense heat of the ground surface in summer stimulates rapid and powerful uplift

5. The world record hailstone fell on the state of Kansas in the USA. It weighed 758 g, that’s 1.7 lbs, and was 7.5 inches in diameter!

6. Here in Britain our contender for the championship fell on Horsham in West Sussex in 1958 and weighed a mere 141 g!

7. What makes a hailstone? What are the special mechanisms? Well, first of all the structure of a cumulonimbus cloud has three distinct layers. At the very top where temperatures are as low as -30 or 40 degrees Celsius the cloud is composed of tiny ice crystals. Near the base of the cloud where the temperatures are probably above freezing minute water droplets are found.

8. Between these two layers is the important zone. Here ice crystals exist with ‘supercooled’ droplets. These are minute water droplets at a temperature below 0 degrees Celsius!

9. Inside the cumulonimbus cloud are powerful up and down currents, caused by the convective turning of air heated by the earths surface. A growing hailstone spends some time in the cloud being cycled between the different layers of the cloud, adding layers of clear ice as droplets freeze on to it, and white ice as ice crystals are attracted.

10. A true hailstone has several of these layers and the number of layers and therefore size of the hailstone depends on the time it has spent being rotated between the different parts of the cloud.

11. In April 1999 in Sydney hail caused one of Australia's costliest natural disasters. Hailstones the size of grapefruit damaged 200,000 homes and ruined 60,000 cars!

12. No deaths were recorded, only cuts and bruises, but in places the hailstones were 20 inches deep on the ground, that’s around half a metre!