EARTH 108 Lecture Notes - Lecture 10: Fujita Scale, Mesocyclone, Vertical Draft

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Lecture outline: tornado formation, supercells & mesocyclones, fujita tornado scale, where & when, tornadoes & climate, mescoscale convective systems. Tornadoes form from high-wind shear and strong updrafts. Warm, humid air near ground collides with cold, dry air at a height. Tornado size (fujita scale) is based on damage assessments. Enhanced fujita scale: named after ted fujita (u chicago, based on fujita scale (1971, enhanced in 2007, ef0 ef5, based on damage assessments, roughly corresponds to wind-speed. A system producing severe thunderstorms and featuring rotating winds sustained by a prolonged updraft that may result in hail or tornadoes. It is a thunderstorm that is contains a mesocyclone (a deep rotating updraft). Supercells have three classification types: classic, low precipitation and high. Supercells that are low precipitation are usually found in drier climates (plains of. Supercells that are high precipitation are often found in moist climates.

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