#27 Postby Derecho » Wed Aug 18, 2004 7:55 pm
And the convection is basically now gone, of course.
When I figured out there was 1 TC forming every four years in the BOC, I used a fairly liberal definition of the BOC extending a few degrees N of the Yucatan.
Had I used the strict definition as that part that is S of the Northern Tip of the Yucatan, it would have been probably one storm forming every 7 or 8 years in the BOC.
There flat out isn't enough room there. While it's one of the classic areas in the Atlantic basin for somtehing to get "Stuck" (witness Roxanne in 1995....which didn't actually FORM in the BOC, though) there usually is at least some Easterly or SE flow.
Whenever the cloud is over the BOC that starts the weekly "All eyes on the BOC!" thread occurs, even if it actually was going to form a TC it typically has all of 6-12 hours, at most, over water. Anything that hasn't formed is likely to be guided by the low-level flow and really has a difficult time staying over water.
I really think it was Bret that may have started the whole BOC-staring thing. But a rare, rare storm, not the norm.
Almost all "BOC" storms actually become at least TDs in the Western Caribbean (including Opal, which became a TD in the Western Carribean, believe it or not) and move there.
Last edited by
Derecho on Wed Aug 18, 2004 7:59 pm, edited 1 time in total.
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