000 AXNT20 KNHC 061735 TWDAT TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 105 PM EST FRI FEB 06 2009 TROPICAL WEATHER DISCUSSION FOR NORTH AMERICA...CENTRAL AMERICA...GULF OF MEXICO...CARIBBEAN SEA...NORTHERN SECTIONS OF SOUTH AMERICA...AND ATLANTIC OCEAN TO THE AFRICAN COAST FROM THE EQUATOR TO 32N. THE FOLLOWING INFORMATION IS BASED ON SATELLITE IMAGERY...METEOROLOGICAL ANALYSIS...WEATHER OBSERVATIONS...AND RADAR. BASED ON 1200 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 1715 UTC. ...THE ITCZ... ITCZ IS CENTERED ALONG 6N7W 1N18W CROSSING THE EQUATOR NEAR 40W AND INTO NE BRAZIL NEAR 2S46W. ISOLATED MODERATE CONVECTION IS FROM 1N-3N BETWEEN 45W-51W. ...DISCUSSION... GULF OF MEXICO... A STRONG 1036 MB SURFACE HIGH PRESSURE CENTERED OVER NE FLORIDA DOMINATES THE PATTERN ACROSS THE GULF. FAIR WEATHER PREVAILS ON S-SE RETURN FLOW ACROSS THE ENTIRE BASIN...WHICH IS ENHANCED BY WIDESPREAD STABILITY ALOFT. THIS IS PRIMARILY CAUSED BY UPPER CONFLUENCE BETWEEN A TROUGH TO THE NE AND A RIDGE TO THE SE. THE SURFACE HIGH IS EXPECTED TO DRIFT E OVER THE NEXT COUPLE OF DAYS AS THE NEXT LOW PRESSURE SYSTEM DEVELOPS OVER THE SRN PLAIN STATES... GRADUALLY INCREASING ELY WINDS OVER THE STRAITS OF FLORIDA AND SELY WINDS ACROSS THE WRN GULF THIS WEEKEND INTO EARLY NEXT WEEK. CARIBBEAN SEA... A STATIONARY FRONT EXTENDS FROM THE W-CENTRAL ATLC INTO THE CARIBBEAN THROUGH THE MONA PASSAGE ALONG 16N70W 14N74W 10N77W. SCATTERED SHOWERS ARE WITHIN 60 NM ON EITHER SIDE OF THE FRONT WITH NE WINDS OVER THE WRN CARIBBEAN. E OF THE FRONT...A SWIFT MOVING SURFACE TROUGH IS ANALYZED FROM 20N61W ACROSS THE LESSER ANTILLES TO THE GULF OF PARIA. THIS SURFACE TROUGH IS EMBEDDED WITHIN FRESH TRADES AND IS PROVIDING THE ERN CARIBBEAN WITH ISOLATED SHOWERS FROM 13N-17N. MOST OF THIS MOISTURE IS SHALLOW IN NATURE AND CAPPED BY A DRY ATMOSPHERE AS OBSERVED IN UPPER AIR SOUNDINGS AND WATER VAPOR IMAGERY. THE FRONT IS EXPECTED TO WEAKEN OVER THE NEXT 24 HOURS ALLOWING WINDS TO DIMINISH GRADUALLY THROUGH THE WEEKEND. ATLANTIC OCEAN... AN DEEP LAYER TROUGH IS ACROSS THE NW ATLC OFF THE COAST OF NEWFOUNDLAND AND SUPPORTS A COLD FRONT THAT ENTERS THE DISCUSSION AREA NEAR 32N53W TURNING STATIONARY NEAR 30N55W AND EXTENDING SW TO THE MONA PASSAGE THEN INTO THE CARIBBEAN SEA. LOW-LEVEL CONVERGENCE OF NW SURFACE WINDS ACROSS THE W ATLC AND E-SE TRADES ACROSS THE CENTRAL ATLC ARE GENERATING SCATTERED SHOWERS WITHIN 150 NM W OF THE BOUNDARY. E OF THE FRONT...DEEP LAYER UPPER RIDGING IS ACROSS MUCH OF THE CENTRAL ATLC WITH THE ASSOCIATED 1032 MB SURFACE HIGH CENTERED NEAR 33N37W. A HIGHLY AMPLIFIED ELONGATED TROUGH LIES SE OF THE RIDGE OVER MUCH OF THE E ATLC. THIS FEATURE IS PROMOTING AN UPPER DIFFLUENT PATTERN AS A SWLY UPPER JET LIES E OF THE BASE OF THE TROUGH AND EXTENDS NE ACROSS WRN AFRICA...DRIVING MIDDLE TO HIGH LEVEL CLOUDINESS WITH POCKETS OF DEEPER MOISTURE S OF 20N E OF 35W. $$ HUFFMAN