Dean4Storms wrote:Wow, convection moving out more like outflows in the NW quadrant.
Yep. One massive outflow boundary.

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Dean4Storms wrote:True Aric, but if it decouples like that it is through.
Aric Dunn wrote:81 hour drifing over central bahamas.. trough quickly lifting out.
Hurricaneman wrote:Dean4Storms wrote:True Aric, but if it decouples like that it is through.
I would say so too, but Jeanne did this exact scenerio in 2004 and hit Florida as a 125mph hurricane, so while I'm not expecting anything close to that but it can't be discounted especially if it has a vigorous 850 to 500 circulation still somewhat in tact
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NDG wrote:More proof that it still has a small closed circulation, perhaps not as strong as earlier today.
CLICK HERE
Stormtrackerjoe wrote:Usually that is not a good sign wrt to intensification, is it not?
Hurricaneman wrote:This is depicting a really badly sheared system, surface low over Florida while the other level lows are 200 miles to the east
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ozonepete wrote:Stormtrackerjoe wrote:Usually that is not a good sign wrt to intensification, is it not?
It depends. If the outflow boundary and all of the area behind it quickly erupts with deep convection (as has been happening with Chantal today) then it doesn't mean anything. It's when outflow boundaries get produced and no new convection fires up near them that one should suspect dry air is winning out.
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