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This Concept Map, created with IHMC CmapTools, has information related to: Upper Level Support 06 Apr 2000, Jet Streaks very Important for Frontal Development, Upward Verical Motion very Important for Cyclone Development, Upper Level Support common feature of CAA Aloft, Upper Level Support Critical for Jet Streaks, Upper Level Support very Important component is Upper Level Divergence, Jet Streaks accelerates Upward Vertical Motion, Upward Verical Motion very Important for Thunderstorm Development, Upper Level Divergence occurs downstream from Upper Level Trough, CAA Aloft creates Upper Level Height Falls, Upper Level Divergence produces Upward Verical Motion, Jet Streaks cause Updrafts to tilt, Jet Streaks very Important for Cyclone Development, Upper Level Height Falls produces Unstable Atmosphere, Jet Streaks exhaust Thunderstorms, TS Development of Short Duration, A Vorticity Maximum may enhance TS Development, Jet Streaks very Important for Thunderstorm Development, Updrafts to tilt causing Updraft to remain Precipitation free, Upper Level Support may produce A Vorticity Maximum, Upward Verical Motion very Important for Frontal Development