These regions have the most frequent and intense mesoscale convective systems.
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These storms have a warm core, like other mesoscale convective systems.
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Most mesoscale convective systems develop overnight and continue their lifespan through the next day.
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Mesoscale convective systems bring 30 to 70 percent of the annual warm season rainfall to the Plains.
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The torrential rains were caused by large clusters of thunderstorms known in meteorological circles as mesoscale convective systems.
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A multicellular storm can sometimes develop into a Mesoscale Convective System ( MCS ) or be a squall line.
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During the summer and early fall, mesoscale convective systems can move into the area from Canada and the Great Lakes.
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A southerly low level jet in the Great Plains of North America helps fuel overnight thunderstorm activity, normally in the form of mesoscale convective systems.
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There was a mesoscale convective system in the area at the time, and the aircraft had deviated to the left of its course to avoid it.
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Mesoscale convective systems are important to the United States rainfall climatology over the Great Plains since they bring the region about half of their annual warm season rainfall.
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