caribepr wrote:The road to Sian Ka'an - south of Tulum
Posted by: Daughter (IP Logged)
Date: July 18, 2005 02:20PM
We just heard from a friend in the area. They had been evacuated to the school. They went down to check property just to the north of Sian Ka'an south of Tulum. The road is barely passable. Some houses are gone, others badly damaged. Their house survived but is without part of the roof. Fences are gone, bushes are gone, trees are defoliaged. There have been no deaths reported in the area.

poof?
Sounds a lot like the damage in Atlanta from the remnants of tropical storm Cindy. So was Cindy a monster too?
What caused the damage in Tulum--sustained winds, tornados, microbursts? If damage associated with tornados or microbursts is often associated with hurricane damage, then wouldn't a tropical storm be just as capable of creating devastating damage as a category 3 hurricane? Why haven't we seen the storm surge damage that we would typically expect to see with a category 4 storm? Why did Dennis produce a significant storm surge so far from his center and we have yet to hear of any significant surge damage with Emily?
These are all questions that come to my mind. Not to incite controversy, but to reach a better understanding of storm dynamics. And, yes, I think Emily went "POOF." Just 12 hours prior to landfall, the NHC was forecasting a 130 kt storm. And, based upon the damage reports which have come in so far, I don't think the 135 mph reported winds at landfall are accurate. I believe the flight level winds were likely accurate, but that the winds were not mixing to the surface.
I'd really like to understand why that happened with Emily--and why that seems to happen quite a bit as storms approach a mainland landfall, and other times just the opposite can happen.