And no raindrop can fall faster than its "terminal speed"--its speed when the downward force of gravity is exactly the same as the upward air resistance. Now, a team of U.S. and Mexican researchers has found that it ain't necessarily so.
Some smaller raindrops can fall faster than bigger ones. In fact, they can fall faster than their terminal speed. In other words, they can fall faster than drops of that size and weight are supposed to be able to fall. And that could mean that the weatherman has been overestimating how much it rains, the scientists say.
"Existing rain models are based on the assumption that all drops fall at their terminal speed, but our data suggest that this is not the case," explains Raymond Shaw, a physicist at Michigan Technological University in Houghton and a member of the research team. "If rainfall is measured based on that assumption, large raindrops that are not really there will be recorded."
understanding of the physics of rain and improve the accuracy of weather measurement and prediction.
Shaw, Alexander Kostinski, also of Michigan Tech, and Guillermo Montero-Martinez and Fernando Garcia-Garcia of the Universidad Nacional Autonoma de Mexico (National University of Mexico) in Mexico City, will publish their findings Saturday, June 13, in the American Geophysical Union's journal, Geophysical Research Letters.
To study the raindrops, they used optical array spectrometer probes and a particle analysis and collecting system. They also modified an algorithm, or computational formula, to analyze raindrop sizes.
The scientists found clusters of raindrops falling faster than their terminal speed, and as the rainfall became heavier, they saw more and more of these unexpectedly speedy drops. Images revealed that the "super-terminal" drops come from the break-up of larger drops, which produces smaller fragments all moving at the same speed as their parent raindrop and faster than the terminal speed predicted by their size.
"In the past, people have seen indications of faster-than-terminal drops, but they always attributed it to splashing on the instruments," Shaw says. He and his colleagues took special precautions to prevent such interference, including collecting data only during extremely calm conditions.
This research was supported in part by the National Science Foundation.Title:
Alexander B. Kostinski: Department of Physics, Michigan Technological University, Houghton, Michigan, USA;
Raymond A. Shaw: Department of Physics, Michigan Technological University, Houghton,Michigan, USA;
Fernando Garcia-Garcia: Posgrado en Ciencias de la Tierra y Centro de Ciencias de la Atmosfera, Universidad Nacional Autonoma de Mexico, Circuito de la Investigacion Cientifica, Mexico City, Mexico.Citation:
Res. Lett., 36, L11818, doi:10.1029/2008GL037111.
Peter Weiss | American Geophysical Union
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