With drought parching the West, seeding clouds for snow is more important than ever. Could this team of scientists prove it really works?
THE RESEARCHERS HAD ALREADY DONE FOUR FLIGHTS, EARLIER in January, before they saw the first hints of what they were looking for. The crew of meteorologists, atmospheric scientists, and students had converged near Idaho’s Snake River Basin, a horseshoe-shaped depression between ranges of the Rocky Mountains that is 125 miles at its widest point. Most of the state’s famous spuds come from this arable land. Each day that the weather was right—clouds containing the perfect amount of super-cooled moisture at the ideal temperature and altitude— the team flew up into the fluff, dropped silver iodide, and watched to see if they were making more snow than there would’ve been if they’d stayed home and hung on to their silver.
It’s called cloud seeding. And people have been planting little chemical seeds into puffy white masses, hoping to change the weather, for some 70 years. But after all that time, no one knows for sure how well it actually works: when or even if the practice makes more snow fall, or how. That’s what the team behind SNOWIE—an acronym for Seeded and Natural Orographic Wintertime clouds: the Idaho Experiment—had come to find out.
“These questions have been around since it started,” says Bob Rauber, one of SNOWIE’s principal investigators and a professor of atmospheric science at the University of Illinois at Urbana Champaign. He has been studying the phenomenon since the ’70s. Today, even though scientists have a computer model that theoretically calculates for success, “we don’t know if it’s right because we haven’t been able to validate it,” he says.
This story is from the July - August 2017 edition of Popular Science.
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This story is from the July - August 2017 edition of Popular Science.
Start your 7-day Magzter GOLD free trial to access thousands of curated premium stories, and 9,000+ magazines and newspapers.
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