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Mesocyclone’s Effect: Supercell Towers Over the Carolinas

Image: An image taken from NASA’s ER-2 aircraft shows a supercell towering 50,000 feet over North Carolina
An image taken from NASA’s high-flying ER-2 aircraft shows the overshooting top of a supercell towering 50,000 feet over North Carolina. The image was taken as the ER-2 flew at 65,000 feet. NASA Earth Observatory

Swirling supercell thunderstorms brewed over the border between North and South Carolina in May, showering the area with chunks of hail as big as baseballs. The huge storm column stretched 50,000 feet (15,000 meters) tall. NASA's Earth Observatory recently released a photo that a pilot took as he flew an ER-2 aircraft over the storms on May 23. Normal commercial airplanes fly at around 30,000 feet (9,000 m), but the ER-2 soared around 65,000 feet (20,000 m).

An anvil-shaped cloud typically forms in a thunderstorm when cooler winds push warm air up into the atmosphere, and a particularly powerful updraft can produce a huge dome-shaped cap called an "overshooting top." Severe storms, like the supercell in the photo, tend to have large and long-lasting overshooting tops. A spinning vortex of air called a mesocyclone lies at the heart of a supercell. When the mesocyclone interacts with strong updrafts, the storms can churn out tornadoes and produce destructive hailstorms. Most of the supercells over the Carolinas in May produced quarter-size hail, but some of the strongest storms rained down baseball-size pieces.

— Kelly Dickerson, LiveScience

This is a condensed version of an article that appeared on Live Science. Read the entire story here. Follow us @livescience, Facebook & Google+.