This story is from the category Libraries and Components
Date posted: 20/07/2009
For generations, schoolchildren have been taught that raindrops start as micro-droplets that then gather together in clouds with their neighbours to become bigger droplets.
Complex interaction between these droplets as they fall explains why raindrops come in such a remarkable range of sizes, goes this idea.
But French scientists armed with ultra-fast video footage say something else happens on the way down -- and this is why rainfall can range from fine droplets to chubby plops.
Initially, a raindrop starts to fall as a sphere, but then flattens out into a pancake shape.
Eventually, as the pancake widens and thins, the onrush of air causes it to hollow out, like an upturned bag.
The bag then inflates beyond the ability of the water's tension to hold things together and bursts into lots of smaller droplets.
The whole process takes only several thousands of a second.
But when the droplets hit the ground, the most numerous by far are very small, while large drops are comparatively few.
"Rainfall does indeed start through coalescence in the clouds but something quite different happens on the way down, and this explains the diversity of raindrop sizes," said Emmanuel Villermaux, who co-wrote the study with Benjamin Bossa of the Aix-Marseille University in southern France.
"Each drop breaks up individually, independently of its neighbours, on its way to earth."
See the full Story via external site: www.physorg.com
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