QUOTE (jfar57 @ Aug 6 2010, 09:33 AM)

The question I have always had relative to Terry's point is about the impact on the water temp. As strong storms come through, they churn the water and bring up the cooler bottom water...right. That mixing must result in some cooling at least. So first question is how significant is that impact? Does the cool water simply turn into a 5 mile wide ribbon thats a degree or three cooler (which is probably inconsequential given the unlikely occurrance of a storm following that same path), or is it more substantial?
Second question is pretty dependent upon first. If there really is a substantial impact, say a 500 mile swath of water that is a few degrees cooler, wouldn't it follow that if we have a few smaller storms early in the year it should lessen the water temp and thus the available fuel? Or the converse, with no churning, does the water warm to such a degree that it really becomes potent fuel for late season devastating storms?
If that was the case you'd never have been able to have the huge storm season we had in 2005 as so many of those storms traversed the same area. The upwelling of cooler water only happens if a storm is stalled and sits over the same area for many days. The famous Cat 5 Hurricane Mitch did this. Otherwise the trop waters stay very even or if they drop off a degree or two with a slower moving storms passage they get it right back before the next storm passes through.
BTW - I've seen a number of posts here of folks impressed with trop waves rolling off Africa, probably anticipating a strong storm from it. A more intense wave coming off the continent is not impressive to me at all. In fact it's usually the death knell of the system from my experience. Typically they will turn north into colder water very early and fizzle right out if they emerge off the coast too strong. You want weaker waves that roll off Africa and d'ont come together until they reach the warmer waters. This is how the monsters like Camille, Katrina, Andrew and Rita developed. Gloria was also similar. Of course any strong Bermuda HP will likely push them far south into the Carribean or below Florida. Other things that are the death knell to hurricanes are any ULL's in the tropics and any east coast trough. The ULL will shear it to death and the trough will either do that or curve it up the middle of the ocean before it reaches the shear area.