When it hails, ever wanted to run out and catch it?
You might not be so keen if the hail was this big!

No exaggeration - hailstones can get this large. But what makes them so big?
Well, it's important to understand why hail falls in the first place. Clouds are full of water vapour which gathers into tiny droplets around pieces of dust in the atmosphere.
They then form bigger droplets until they fall, as rain!
But sometimes, conditions change. There are winds, or updrafts, which travel upwards in the clouds, and are able to stop the raindrops from moving downwards.
The updrafts also move the raindrops upwards in their clouds.

Demonstration time - assuming this piece of sponge is a piece of dust, it gets a layer of water...
...then moves up to the top of the cloud.

The higher it goes, the colder it becomes.

This is where the raindrop freezes.
It then becomes a baby hailstone, and it falls back down within the cloud.
Here it warms up and picks up another layer of water. It zooms up again...
...and freezes once more. The more often this happens, the bigger the hailstone becomes!
Eventually it becomes so large, the updrafts can no longer support it, and it falls out of the sky to the ground.
Because of all the freezing and thawing, hailstones are layered, just like gobstoppers.

Check out the layers inside this one!
The world record for the biggest hailstone is 1kg in weight.

It was recorded as falling in Bangladesh in 1986!
So the next time you're tempted to run out and play in a hailstorm, you might want a hard hat!
© BBC MMI

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