Flareup in NW Caribbean

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boca
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Flareup in NW Caribbean

#1 Postby boca » Tue Feb 07, 2006 8:11 am

I know its not tropical in nature. Its the tail end of the old front that came thru Florida this past weekend. Still impressive to have a flareup like that in Feb.
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#2 Postby HURAKAN » Tue Feb 07, 2006 8:25 am

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Very high shear values in the area.
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#3 Postby LaBreeze » Tue Feb 07, 2006 10:05 am

Thankfully it's not August or September.
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#4 Postby HURAKAN » Tue Feb 07, 2006 11:37 am

Image

THIS IS WHAT IS VISIBLE FROM CUBA'S CLOSEST RADAR TO THE AREA OF CONVECTION.
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Coredesat

#5 Postby Coredesat » Tue Feb 07, 2006 12:27 pm

THE STATIONARY FRONT FROM THE W/CENTRAL ATLC ENTERS THE
CARIBBEAN THROUGH THE WINDWARD PASSAGE EXTENDING WSW JUST W OF
JAMAICA ALONG 18N80W TO OVER HONDURAS NEAR 15N86W. OVERCAST LOW
CLOUDS ARE W OF THE FRONT WITH SCATTERED SHOWERS/THUNDERSTORMS
BETWEEN 17N-21N FROM 80W TO JUST INLAND OVER THE YUCATAN
PENINSULA.

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#6 Postby JonathanBelles » Tue Feb 07, 2006 2:08 pm

development or no?
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#7 Postby KWT » Tue Feb 07, 2006 2:20 pm

No i'd have thought not, shear is high in that region and it doesn't look even slightly organised, its just a convective flare-up as has already been said. Now in summer and under better shear values...who knows!
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Coredesat

#8 Postby Coredesat » Tue Feb 07, 2006 2:22 pm

It's just cutoff convection. There's no low pressure area or circulation, and there's too much dry air and shear for any development.
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#9 Postby mike815 » Tue Feb 07, 2006 4:07 pm

yeah way to dry still wow
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