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Este Cmap, tiene información relacionada con: Upper Level Support 06 Apr 2000, Updrafts to tilt causing Updraft to remain Precipitation free, Upward Verical Motion very Important for Thunderstorm Development, Jet Streaks very Important for Thunderstorm Development, Jet Streaks accelerates Upward Vertical Motion, CAA Aloft creates Upper Level Height Falls, TS Development of Short Duration, Upper Level Support may produce A Vorticity Maximum, Upper Level Support very Important component is Upper Level Divergence, Jet Streaks cause Updrafts to tilt, Upper Level Support Critical for Jet Streaks, Upper Level Divergence occurs downstream from Upper Level Trough, Upper Level Divergence produces Upward Verical Motion, Upward Verical Motion very Important for Frontal Development, Jet Streaks very Important for Frontal Development, Jet Streaks exhaust Thunderstorms, A Vorticity Maximum may enhance TS Development, Jet Streaks very Important for Cyclone Development, Upward Verical Motion very Important for Cyclone Development, Upper Level Height Falls produces Unstable Atmosphere, Upper Level Support common feature of CAA Aloft