Below is the 1:05 PM discussion from TPC.
THE CARIBBEAN SEA...
A FAIRLY SHARP AIRMASS DIFFERENCE EXISTS IN THE CARIB. THE
DIVIDER IS A STRONG COLD FRONT WHICH EXTENDS FROM THE ATLC
ACROSS THE BAHAMAS/ERN CUBA EXTENDING SWD TOWARDS THE COAST OF
PANAMA NEAR 10N82W. BEHIND THE FRONT...COOLER AND NOTABLE DRIER
AIR IS ADVECTED INTO THE REGION ON STRONG NLY WINDS. THESE WINDS
HAVE REACHED GALE FORCE S OF 18N BETWEEN 80W-85W. STRONG WINDS
AND HIGH SEAS ARE ALSO REPORTED FROM SHIPS IN THE YUCATAN
CHANNEL. FOR MORE DISCUSSION ON THIS UNSEASONABLE AIRMASS REFER
TO THE GULF OF MEXICO SECTION AND FOR WINDS AND SEAS REFER TO
MIAOFFNT3 AND MIAOFFNT4. ACTIVE WEATHER...IN TERMS OF SHOWERS
AND TSTMS...LIES TO THE E OF THE FRONT. A PRE-FRONTAL TROUGH IS
ANALYZED ABOUT 120-150 NM AHEAD OF THE FRONT FROM THE SE BAHAMAS
SWD ALONG 17N76W 13N79W TO PANAMA. SFC OBSERVATIONS AND VIS
IMAGES INDICATE A WIND SHIFT AND LINE OF LOW-LEVEL CONVERGENCE
WHICH WAS THE REASON OF ANALYZING THIS FEATURE AHEAD OF THE MAIN
BOUNDARY. SCATTERED SHOWERS AND TSTMS ARE WITHIN 150 NM AHEAD OF
THE FRONT. HOWEVER MORE IMPRESSIVE ACTIVITY...NUMEROUS MODERATE
CONVECTION...IS NEAR THE BASE OF THE FRONT S OF 13N BETWEEN
75W-82W. NUMEROUS MODERATE IS ALSO AHEAD OF THE TROUGH/FRONT
FROM 12N-18N BETWEEN 72W-76W. SOME OF THIS STRONGER ACTIVITY IS
BEING ENHANCED BY UPPER LEVEL DIFFLUENCE BETWEEN A HIGHLY
AMPLIFIED STRETCHED UPPER RIDGE AND THE STRONG TROUGHING ACROSS
THE SW ATLC/GULF AND NW CARIB. THE ERN CARIB IS QUIET WITH UPPER
LEVEL CONFLUENCE PRODUCING PLENTY OF DRY STABLE UPPER LEVEL AIR
E OF 69W. GFS SHOWS THE DEEP MOISTURE SWATH REMAINING NEARLY
STATIONARY BUT SHRINKING IN SIZE AND GRADUALLY WEAKENING OVER
THE NEXT COUPLE DAYS IN THE CNTRL/WRN CARIBBEAN.
http://www.storm2k.org/wx/modules.php?n ... ge&pid=109
TheEuropean,there is no low now according to the latest discussion.