something to watch?
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JamesFromMaine2
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Re: something to watch?
JamesFromMaine2 wrote:Any chance anything will develop out of this?
With 60 knots shear, Id say not.
http://cimss.ssec.wisc.edu/tropic/real-time/atlantic/winds/wg8shr.html
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gpickett00
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Please tell me you're kidding.-
Audrey2Katrina
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gpickett00 wrote:it wont develop because its not hurricane season
Well has anyone told this wave that? ROFL...
Anyway... all kidding aside, they HAVE had tropical cyclones in every month of the year; but I concur with another poster. Conditions don't look favorable for much development; but I'm sure that should anything develop, this'll be the place to find out about it.
A2K
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Margie
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JamesFromMaine2
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ATLANTIC OCEAN...
COLD FRONT OVER THE W ATLC EXTENDS FROM 32N54W TO JUST N OF
DOMINICAN REPUBLIC NEAR 21N69W. WIDELY SCATTERED TSTMS ARE
WITHIN 60 NM OF THE FRONT N OF 26N DUE TO AN UPPER SHORTWAVE
NEAR 31N56W THAT IS ENHANCING UPPER LIFT. ONLY ISOLATED SHOWERS
ARE N OF 22N AND COLD AIR STRATOCUMULUS ARE BEHIND THE FRONT TO
73W. LARGE UPPER TROUGH OVER THE W ATLC IS PROVIDING THE PUSH
FOR THE FRONT THOUGH IT IS WEAKENING. 1031 MB HIGH IS N OF THE
AREA JUST SW OF THE AZORES WITH STRONGER TRADES THAN AVERAGE IN
THE E ATLC E OF 50W. THE TROPICAL ATLC CONTINUES TO BE RATHER
QUIET W OF 40W AS MODERATE/STRONG SUBSIDENCE DOMINATES. HOWEVER
AN UPPER LOW NEAR 19N38W IS PRODUCING A LARGE AREA OF CLOUDS E
OF 38W WITH A WEAK SURFACE TROUGH REFLECTION FROM 8N33W 16N34W.
OVERCAST HIGH CLOUDS WITH EMBEDDED POCKETS OF SHOWERS/TSTMS ARE
E OF 36W TO W AFRICA BETWEEN 8N-22N WITH THE DEEPEST CONVECTION
WITHIN 120 NM OF 18N33W. MODELS INDICATE THIS AREA OF DISTURBED
WEATHER SHOULD CONTINUE OVER THE REGION AND DRIFT WESTWARD WITH
THE UPPER LOW. OTHERWISE THE ITCZ IS FAR TO THE SOUTH IN THE
REGION.. ABOUT AVERAGE FOR THIS TIME OF YEAR. UPPER RIDGING
COVERS THE CENTRAL ATLC BETWEEN THE UPPER TROUGH/LOW AND E OF
THE UPPER LOW. WEAK COLD FRONT IS IN THE FAR NE PART OF THE
REGION NEAR THE CANARY ISLANDS PRODUCING SOME RAIN SHOWERS IN
THOSE ISLANDS.
COLD FRONT OVER THE W ATLC EXTENDS FROM 32N54W TO JUST N OF
DOMINICAN REPUBLIC NEAR 21N69W. WIDELY SCATTERED TSTMS ARE
WITHIN 60 NM OF THE FRONT N OF 26N DUE TO AN UPPER SHORTWAVE
NEAR 31N56W THAT IS ENHANCING UPPER LIFT. ONLY ISOLATED SHOWERS
ARE N OF 22N AND COLD AIR STRATOCUMULUS ARE BEHIND THE FRONT TO
73W. LARGE UPPER TROUGH OVER THE W ATLC IS PROVIDING THE PUSH
FOR THE FRONT THOUGH IT IS WEAKENING. 1031 MB HIGH IS N OF THE
AREA JUST SW OF THE AZORES WITH STRONGER TRADES THAN AVERAGE IN
THE E ATLC E OF 50W. THE TROPICAL ATLC CONTINUES TO BE RATHER
QUIET W OF 40W AS MODERATE/STRONG SUBSIDENCE DOMINATES. HOWEVER
AN UPPER LOW NEAR 19N38W IS PRODUCING A LARGE AREA OF CLOUDS E
OF 38W WITH A WEAK SURFACE TROUGH REFLECTION FROM 8N33W 16N34W.
OVERCAST HIGH CLOUDS WITH EMBEDDED POCKETS OF SHOWERS/TSTMS ARE
E OF 36W TO W AFRICA BETWEEN 8N-22N WITH THE DEEPEST CONVECTION
WITHIN 120 NM OF 18N33W. MODELS INDICATE THIS AREA OF DISTURBED
WEATHER SHOULD CONTINUE OVER THE REGION AND DRIFT WESTWARD WITH
THE UPPER LOW. OTHERWISE THE ITCZ IS FAR TO THE SOUTH IN THE
REGION.. ABOUT AVERAGE FOR THIS TIME OF YEAR. UPPER RIDGING
COVERS THE CENTRAL ATLC BETWEEN THE UPPER TROUGH/LOW AND E OF
THE UPPER LOW. WEAK COLD FRONT IS IN THE FAR NE PART OF THE
REGION NEAR THE CANARY ISLANDS PRODUCING SOME RAIN SHOWERS IN
THOSE ISLANDS.
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