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October 18, 2004

No hail, no sleet on I-95. It was "graupel."

Several poor souls caught in that wild storm on Interstate 95 at about 4:30 p.m. Saturday described the ice that pelted their windshields as "sleet." The National Weather Service called it "pea-sized hail." But meteorologist Jeff Warner, of Penn State Weather Communications, said it was neither. He called it "graupel." Whatever it was, it combined with rain, sun glare and steam rising off the pavement to turn the highway into a demolition derby - at least 17 multi-car collisions, involving more than 90 vehicles. Several people were injured, but thankfully, there were no fatalities.

Warner said hail forms in thunderstorms when ice crystals high in the atmosphere contact super-cooled water. The water turns to ice and the hail stone grows. It grows until it's too large and heavy to stay aloft in the storm's powerful updrafts. The storm on Saturday, Warner says, wasn't a thunderstorm.

Sleet forms in winter when a warm air mass runs up and over a cold air mass. As its moisture rises, it cools, forming snowflakes, which fall toward the surface. When they hit the warm air layer, however, the flakes melt. Then, as they hit the cold air near the surface, they refreeze and form hard ice pellets. None of that applied on Saturday, Warner said.

Graupel is sometimes called "soft hail." It forms in strong cold fronts, like the one on Saturday. The air above 5,000 feet was near freezing, he said, and snow formed. When it reached warmer air below about 5,000 feet, the flakes partially melted and stuck together. Caught in updrafts, they merged with water droplets and formed a sort of "soft" or "squishy" ice pellet.

Warner said State College, Pa. also saw an intense graupel shower at about 3 p.m. Saturday. It's fairly common in the lee of the Great Lakes when intense cold fronts sweep off the lakes but it's not yet cold enough to cause "lake effect" snows. It's much more unusual this far south and east.

He called Saturday's event a "typical autumn cold front with a sharp temperature gradient." Winds at Martin State Airport at 3:45 p.m. were out of the southwest at a lazy 7 mph, with temps at 63. Two hours later the winds were from the west at 15 mph, with gusts to 26, and temperatures had fallen 13 degrees, to 50.

At BWI, temperatures fell 11 degrees - from 61 to 50 during the same period, with a peak wind gust of 31 mph.

Posted by Admin at 1:47 PM | | Comments (3)
Categories: Events
        

Comments

Warner may not have called it a thunderstorm, but it was certainly one here northwest of Baltimore. There was thunder in both cells on saturday afternoon.

I wondered about that, too. I was out on Locust Point, near Ft. McHenry when that front blew through, and I thought I heard a clap of thunder. Whether that qualifies it as a thunderstorm, and the falling ice as hail, I'm not so sure.

There were multiple cloud-to-ground lighting strikes detected with that particular storm. By the way, we also had large hail and very strong winds in Reston, VA from the storms.

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About Frank Roylance
This site is the Maryland Weather archive. The current Maryland Weather blog can be found here.
Frank Roylance is a reporter for The Baltimore Sun. He came to Baltimore from New Bedford, Mass. in 1980 to join the old Evening Sun. He moved to the morning Sun when the papers merged in 1992, and has spent most of his time since covering science, including astronomy and the weather. One of The Baltimore Sun's first online Web logs, the Weather Blog debuted in October 2004. In June 2006 Frank also began writing comments on local weather and stargazing for The Baltimore Sun's print Weather Page. Frank also answers readers’ weather queries for the newspaper and the blog. Frank Roylance retired in October 2011. Maryland Weather is now being updated by members of The Baltimore Sun staff
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