Downslope Wind Events.

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Presentation transcript:

Downslope Wind Events

Moving up the mountainside, for subcritical flow, ∂u/∂x > 0, so wind speed increases and h decreases. This is consistent with conservation of energy. This opens the potential for Fr approaching 1. If Fr > 1 after the mountain top, then by the equation on the previous slide, ∂u/∂x > 0, and the flow can go faster and faster down the mountain side, which can make Fr yet more positive. Consistent with energy conservation, h continues to decrease, which makes c decrease further, also making Fr more positive. Eventually, a hydraulic jump occurs and turbulence is generated, which leads to lee mountain waves.