On a Caribbean collision course?
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- dixiebreeze
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On a Caribbean collision course?
http://www.ssd.noaa.gov/goes/east/watl/rb-l.jpg
Some action in the western and upper central Caribbean might just decide to get together. Is that a possibility in anyone's mind?
Some action in the western and upper central Caribbean might just decide to get together. Is that a possibility in anyone's mind?
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Re: On a Caribbean collision course?
I see that but it's too close to Central America to say anything right now.
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- 'CaneFreak
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- dixiebreeze
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- cycloneye
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Re: On a Caribbean collision course?
If convection persists for 24 hours then a more closer look has to occur.


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- lrak
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Re: On a Caribbean collision course?
What is that spin fixing to head under those super cells off the coast of Nicaragua...93L or is it futher back? Looks like somethings going to happen, will have to watch it tonight for sure like cycloneye said . The mess off the Nicaraguan coast that is. This little gif below sure is forecasting giant waves off the S.Tx coast at the end of the weekend and I just can't see the blobs under Puerto Rico making it that far that soon, so its got to be these blobs off Nicaragua, eh?
http://www.lajollasurf.org/images/caanim.gif
http://www.lajollasurf.org/images/caanim.gif
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- cycloneye
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Re: On a Caribbean collision course?
From 8 PM Discussion:
TROPICAL WAVE IS OVER THE WESTERN CARIBBEAN ALONG 84W S OF 16N
MOVING W 15 KT. THIS WAVE LIES IN AN UPPER DIFFLUENT ZONE ON
THE S SIDE OF AN UPPER HIGH. THESE TWO FEATURES TOGETHER ARE
PRODUCING SCATTERED MODERATE TO STRONG CONVECTION ALONG THE
COASTS OF HONDURAS AND NICARAGUA FROM 13N-18N BETWEEN 80W-85W.
TROPICAL WAVE IS OVER THE WESTERN CARIBBEAN ALONG 84W S OF 16N
MOVING W 15 KT. THIS WAVE LIES IN AN UPPER DIFFLUENT ZONE ON
THE S SIDE OF AN UPPER HIGH. THESE TWO FEATURES TOGETHER ARE
PRODUCING SCATTERED MODERATE TO STRONG CONVECTION ALONG THE
COASTS OF HONDURAS AND NICARAGUA FROM 13N-18N BETWEEN 80W-85W.
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- deltadog03
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- 'CaneFreak
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Re: On a Caribbean collision course?
cycloneye wrote:From 8 PM Discussion:
TROPICAL WAVE IS OVER THE WESTERN CARIBBEAN ALONG 84W S OF 16N
MOVING W 15 KT. THIS WAVE LIES IN AN UPPER DIFFLUENT ZONE ON
THE S SIDE OF AN UPPER HIGH. THESE TWO FEATURES TOGETHER ARE
PRODUCING SCATTERED MODERATE TO STRONG CONVECTION ALONG THE
COASTS OF HONDURAS AND NICARAGUA FROM 13N-18N BETWEEN 80W-85W.
HMMMMMMMMMMM.....WHO SAID THAT ALL THIS WAS CAUSED BY UPPER LEVEL DIVERGENCE AND THAT DEVELOPMENT WOULD LIKELY NOT OCCUR....hmmmmmm......
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- 'CaneFreak
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Re:
deltadog03 wrote:There is some very good upper level divergance....In another words an upper level anticyclone above that convection.
Yes, but with no low level center trying to develop upper level divergence is like pissing in the wind....it does nothing...
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- cheezyWXguy
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Re: Re:
'CaneFreak wrote:deltadog03 wrote:There is some very good upper level divergance....In another words an upper level anticyclone above that convection.
Yes, but with no low level center trying to develop upper level divergence is like pissing in the wind....it does nothing...
Sure it does, it gets you wet

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Re:
KWT wrote:Convection that was present yesterday has totally decayed and gone poof.
Typical Carribean convection that pulses up for while then diminishes quickly. Probably why it hardly gets mentioned in the TWO.
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