Thursday, 31 August 2006: 10:30 AM
Ballroom South (La Fonda on the Plaza)
An important nonlinear benchmark in our understanding of mountain waves are the exact steady solutions produced by Long's theory. These 2D flows are well-known to be unstable when the topographic heights cause the streamlines to be at, or very close to, overturning. A new mechanism for the instability of steady, hydrostatic mountain waves is identified through the analysis of the linear stability problem. When the topography has multiple peaks, it is shown that the overturning criterion can be superceded by a resonant instability. In particular, for flow over two peaks, the threshold heights for instability are roughly half as high as required for overturning streamlines. The mechanism behind the instability is the parametric amplification of counter-propagating gravity waves. The resonant nature of the instability is further illustrated by the existence of discrete peak-to-peak separation distances where the growth rate is a maximum. This instability mechanism illustrates a dynamical pathway to flow overturning, and the onset of turbulence.
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