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Severe and Unusual Weather ESAS 1115

Severe and Unusual Weather ESAS 1115. Spotter Training and Radar Meteorology Part 4 – Multicell Thunderstorms. Multicell Thunderstorms. Several distinct updraft/downdraft couplets exist Can form as a cluster or a squall line

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Vertical Momentum Eq. (rewritten)

Vertical Momentum Eq. (rewritten). (dynamic) + (buoyancy). …real bubble in 3D simulation. Buoyancy is Scale-Dependent!!!. Basic 2D Equations:. ⁄. --. Or, more simply, consider the 2D horizontal vorticity equation:. where. Buoyant Processes:. Buoyancy is Scale-Dependent!!!.

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340 views • 17 slides

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