Don Moore - WFO Spokane
The stiff sustained winds were a result of a very tight pressure gradient. However, it is likely the higher wind gusts that caused most of the damage were a result of mid level winds accelerating down to the surface. One indication of this is a number of surface observations reporting rapidly a falling pressure, followed by a rapidly rising surface pressure, and then another rapidly falling surface pressure. Water Vapor imagery also indicates that this type of phenomena may be occuring (Fig. 6). Visible imagery also clearly shows the impact of subsidence associated with the short wave trough (Fig. 7).
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