high velocity storms are the results of
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These storms occur when high levels of condensation form in a volume of unstable air that generates deep, rapid, upward motion in the atmosphere. The heat energy creates powerful rising air currents that swirl upwards to the tropopause. Cool descending air currents produce strong downdraughts below the storm.
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High velocity storms are the results of when condensation form in a volume of unstable air that generates rapid and deep and upward motion in the atmosphere.
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