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Summer hail  
 

By Wijke Ruiter
 

"Devastating huge hailstones swept down from heaven above Holland?? I would never have believed it if I hadn't seen it with my own eyes; it happened about 4 years ago. I managed to take a picture through the window. It was the final scene of a thunderstorm passing; well, not a plain, simple Dutch thunderstorm that's for sure. 

It was an imposing one; coming upon us in all ranging colours from white-grey to deep-black; whirling and swirling in a low sky; as if the end of the world was there. No time to feel scared yet; only deeply astonished, nailed to the ground,  just watching; this can't be real. Sudden heavy wind gusts raged along;  rousing: a sense of danger flashed through the mind; we rushed into the house,  just before white tennis-balls plopped on the green. "White tennis-balls"?? It was hailstones."

Damaging hail

Hail in summer; is this normal? Hail showers are quite common over Britain in westerly and northerly airstreams in winter or in early spring; but during the summer there can be hail as well, however not so often and, what's more, the hailstones can be much bigger than in wintertime. 

These bigger hailstones are far more dangerous and can devastate whole area's; damaging everything that's around. There are places on earth where large hailstones are quite common; mostly regions where tornado's are active, or in tropical and sub-tropical countries. Wine-  and orange growers in Italy, Spain and France have developed special methods to prevent the demolition of the vintage.
Grenades with silver-iodine are fired into a thunder-cloud. The water-drops in the cloud precipitate on the iodide crystals. The droplets are divided over a huge amount of crystals; whereby every individual ice-crystal will stay smaller. The hailstones that fall down to earth also stay small; a lot of damage has been avoided.

In our regions storms with huge summer-hailstones are quite unusual, but sometimes it can go beyond any control. Chances of hailstones of about 1 inch (2,5 cm) are only a few percent; and chances of stones which are about 1,2 inch (3 cm) are three to five times smaller; but the damage this odd bigger hailstones bring grows very fast with the size. That's due to the bigger mass and the increasing velocity. 
Round stones with a size of 1,2 inch have a speed of 30 mph and stones of 2,5 inch; about 80 mph. Much larger stones can gain a velocity of 200 mph. 

With such a speed, its easy to envisage that these large stones can dent cars; destroy greenhouses, roofs, plants, crops; really everything that's in its way down. People can get injured, and animals, especially birds, can easily be killed in a heavy hailstorm.

Where does hail actually come from?

Large hailstones develop in huge thunderstorm-clouds. These clouds are cumulonimbus clouds. In such a cloud are falling and rising airstreams; called down- and updrafts.  The cloud base may be 2,000 feet above the ground with tops at 30,000 feet. Much of the cloud will be composed of super cooled water droplets. As the hailstone falls it will collect tiny water droplets which freeze and form a layer of ice. Perhaps the hailstone will then be caught in a vigorous updraft. As it is carried back higher into the cloud, it collects more minute water or ice particles to form another layer of ice. Thus layers build up on the hailstone  ice) and the cycle may be repeated until the stone is so big that the updraft can't lift it anymore; and it'll fall to earth.
Sometimes the updraft - and the connecting downdraft - in a thunderstorm is gets impulses of a jet stream at higher altitude. (Jet streams are strong winds at about 9 - 10 kilometer (30.000 - 33.000 feet) high in the atmosphere, with a force of 65 mph or more.) 
When this is the case the up- and downdrafts can be very violent. And really heavy hailstones are easily lifted up again and again. 
Its not hard to imagine that such huge thunderstorms with such severe up- and downdrafts can enlarge enormous hailstones - to the size of tennis-balls.

A hailstone in profile

Now we know how hailstones grow its obvious that the stones consist of layers of ice. These layers are made of alternate opaque and clear ice. In the first case the hailstone within the top of cloud - where its very cold - catches droplets of water that immediately freeze to the stone; in the second case the stone catches water droplets that form a layer of water around the stone; this layer freezes to the stone. In that stadium the stone is down at the bottom of the cloud.
This layers can tell you about the stones history: how often its been lifted by the updraft to the top of the cloud and how often is has fallen down.

Where do these stones fall?

 Almost every summer larger hailstones - of about 1 inch - will fall somewhere in our region but tend to occur mainly in the south of Britain, about four to five times a year.  The largest hailstone recorded in the British Isles weighed 142 grams (5 oz), was about 3 inches, and occurred at Horsham, West Sussex on 5 September 1958. 
The hailstorm described at the top of this special brought extreme huge stones of about 4 inches to Holland on the 6th of June 1998.

 The USA, Canada, central Europe, the southern parts of the CIS, India and China all experience large hail. So too do land areas in the southern hemisphere. The world record (as quoted in the 1994 edition of The Guinness Book of Records) occurred in a hailstorm in the Gopalanj district of Bangladesh on 14 April 1986. The hailstones weighed up to 1 kg (2 lb 4 oz) and were reported to have killed 92 people.

 

 wijke@scribeweekly.com

 
 Pictures from
 Author and The Met Office