Invest 91L,E Caribbean,Comments,Sat Pics,Models Thread #3
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You get pressure drops and wind increases with a sfc trough (wave axis) especially if there is convection present. It does not mean there has to be a LLC.
Sure, but we've been following the surface Low spiral on this one so calling it a trough feature isn't valid.
I've seen this before where the Atlantic easterly flow inhibits or disrupts the return winds on such a weak storm. The west wind sometimes gets cancelled by the strong Atlantic tropical easterly in this area.
That's why I say precise definition doesn't always apply to this level of storm. I think Claudette a few years back also jumped this phase.
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Sanibel wrote:I also go by no one yet explaining a pressure drop and windspeed increase without an LLC.
Especially with such a promising dvorak.
What increase in wind speed? What drop in pressure? If you're going by the NRL estimates, they're estimates, not actual data. Recon is actual data, and there's barely 25 knots at 1010mb at the surface, let alone 35 knots and 1000mb.
Last edited by StormsAhead on Wed Aug 09, 2006 2:04 pm, edited 1 time in total.
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The models were initiaized with a forward motion of 27 knots.
You can prety much forget about anything closing off moving that fast.
This is what the GFS and the related BAM models have been seeing. The lower half is racing along the low level ridge...and the mid level circ is lagging behind...note the possible MLC that was left behind in vis imagery loops.
As long as this business continues...we won't see any development
If it gets a chance to slow down and stack a little bit it has a chance to go.
MW
You can prety much forget about anything closing off moving that fast.
This is what the GFS and the related BAM models have been seeing. The lower half is racing along the low level ridge...and the mid level circ is lagging behind...note the possible MLC that was left behind in vis imagery loops.
As long as this business continues...we won't see any development
If it gets a chance to slow down and stack a little bit it has a chance to go.
MW
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SPECIAL TROPICAL DISTURBANCE STATEMENT
NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL
300 PM EDT WED AUG 9 2006
REPORTS FROM AN AIR FORCE RECONNAISSANCE PLANE INDICATE THAT THE
TROPICAL WAVE NEAR THE LESSER ANTILLES DOES NOT HAVE A CLOSED
SURFACE CIRCULATION. HOWEVER...THE POTENTIAL STILL EXISTS FOR THIS
SYSTEM TO BECOME A TROPICAL DEPRESSION DURING THE NEXT DAY OR SO.
SHOWERS AND THUNDERSTORMS WITH GUSTY WINDS TO TROPICAL STORM FORCE
ARE STILL POSSIBLE AS THE WAVE MOVES ACROSS THE LESSER ANTILLES
TODAY AND TONIGHT.
NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL
300 PM EDT WED AUG 9 2006
REPORTS FROM AN AIR FORCE RECONNAISSANCE PLANE INDICATE THAT THE
TROPICAL WAVE NEAR THE LESSER ANTILLES DOES NOT HAVE A CLOSED
SURFACE CIRCULATION. HOWEVER...THE POTENTIAL STILL EXISTS FOR THIS
SYSTEM TO BECOME A TROPICAL DEPRESSION DURING THE NEXT DAY OR SO.
SHOWERS AND THUNDERSTORMS WITH GUSTY WINDS TO TROPICAL STORM FORCE
ARE STILL POSSIBLE AS THE WAVE MOVES ACROSS THE LESSER ANTILLES
TODAY AND TONIGHT.
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Sanibel wrote:You get pressure drops and wind increases with a sfc trough (wave axis) especially if there is convection present. It does not mean there has to be a LLC.
Sure, but we've been following the surface Low spiral on this one so calling it a trough feature isn't valid.
I've seen this before where the Atlantic easterly flow inhibits or disrupts the return winds on such a weak storm. The west wind sometimes gets cancelled by the strong Atlantic tropical easterly in this area.
That's why I say precise definition doesn't always apply to this level of storm. I think Claudette a few years back also jumped this phase.
The sfc low opened up due to lack of convection. Plus what you are seeing in satellite is most likely a mid level center. Recon has not found anything impressive at all so far.
But what the heck do I know. You must be the expert.

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