btangy wrote:Sidr is very near its potential intensity and just passed over an area of higher than normal ocean heat content. There is some subtle evidence from that the deepest convection is now shifting downshear indicating that the shear is increasing from the S. CIMSS diagnoses the shear at 11m/s from 190 degrees, but the actual shear the storm is experiencing is most likely much less. One can only hope the change in convective signature is the start of a weakening trend.
One problem is that a weakening of the peak wind may not reduce the surge threat. What we've observed time after time is that an intense hurricane that weakens rapidly will retain much of its kinetic energy. Though the peak wind may drop significantly, the wind field expands to compensate. This happened with Katrina and Rita prior to landfall. The resulting expansion in the wind field could mean that the devastating storm surge would cover a larger area. Such a retention of kinetic energy was observed mostly following hurricanes that interacted with land (Wilma near the Yucatan, Katrina passing over Florida) or during eyewall replacement cycles. Weakening due to strong shear may also disrupt the surface wind field, reducing the surge.
In the case of Sidr, it's looking like almost a worst-case scenario. Surge could be in the 20-30 foot range in an area as flat as south Louisiana but with many millions more people.