Tuesday, 25 April 2006: 11:30 AM
Regency Grand Ballroom (Hyatt Regency Monterey)
Presentation PDF (137.1 kB)
It has been previously demonstrated that barotropic instability across the hurricane eyewall results in polygonal features along the eye/eyewall interface and an asymmetric contraction of the eyewall. Using a 2D barotropic numerical model, we will demonstrate a new pathway to these phenomena in the absence of barotropic instability. Relevance to observations in hurricanes will be discussed.
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