#5 Postby Aslkahuna » Mon Oct 30, 2006 1:09 am
I rechecked the 1967 ATCR and Carla peaked at 160kt but was at 100kt when it made landfall. However, it still produced 55kt gusts at Mactan. The important thing to remember about the NE coast of Luzon is that it's a virtual wall to any storm making landfall there-especially the strong storms which are highly organized and in which the inflow is restricted to the levels from H85 down. When the storm hits, the lower levels are shredded apart and the mid levels keep moving. The residual vorticity in the mid level circulation will intiate redevelopment off the west coast of the island as it moves off and the two will recouple and the storm begins to reintensify. So although a storm may make landfall with 155kt winds, they will not last long at all as the storm decouples with the LLCC unable to make over the mountains.
Steve
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