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Wave ducting in a stratified shear flow over a two-dimensional mountain. Part II: Implications for the development of high-drag states for severe downslope windstorms
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ABSTRACT
In this study, it is found that the discrepancies among earlier studies of severe downslope windstorms are caused by the use of the critical level height (z^sub c^) instead of the low-level uniform flow-layer depth (z^sub 1^), as an indicator to determine the optimal conditions for the occurrence of high-drag states. It is determined that once the wave breaking occurs, it induces a critical level and establishes a flow configuration favorable for wave ducting in the lower uniform wind layer, which determines the phase of reflected waves.
Flow regimes of high- and low-drag states ...
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