000 AXNT20 KNHC 041751 TWDAT TROPICAL WEATHER DISCUSSION NWS NATIONAL HURRICANE CENTER MIAMI FL 105 PM EST SUN DEC 04 2011 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...WEATHER OBSERVATIONS...RADAR...AND METEOROLOGICAL ANALYSIS. BASED ON 1200 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 1715 UTC. ...ITCZ/MONSOON TROUGH... THE INTERTROPICAL CONVERGENCE ZONE AXIS EXTENDS FROM 07N11W TO 04N22W TO 05N52W. ISOLATED MODERATE CONVECTION IS WITHIN 45 NM EITHER SIDE OF A LINE FROM 03N26W TO 03N34W. ...DISCUSSION... GULF OF MEXICO... AN UPPER LEVEL RIDGE AXIS EXTENDS FROM THE SW GULF NORTHEASTWARD OVER NORTHERN FLORIDA AND ALONG THE EASTERN U.S. SEABOARD TO BEYOND 32N80W. THIS UPPER LEVEL FEATURE CONTINUES TO SUPPORT A FAIRLY LARGE AND STRETCHED 1039 SURFACE HIGH PRESSURE AREA CENTERED WELL NE OF THE AREA OFF THE COAST OF NOVA SCOTIA NEAR 43N63W. THE SURFACE RIDGE AXIS EXTENDS SW ALONG THE EAST COAST OF THE US...INFLUENCES MUCH OF THE SE CONUS E OF 90W AND EXTENDS OVER MUCH OF THE GULF TO A 1020 MB HIGH CENTERED OVER CENTRAL MEXICO NEAR 20N98W. MODERATE TO FRESH E TO SE WINDS ARE EXPECTED TO PERSIST ON THE SOUTHERN PERIPHERY OF THE HIGH THROUGH MONDAY MORNING. AN UPPER LEVEL TROUGH CURRENTLY MOVING ACROSS ARIZONA AND NORTHWESTERN MEXICO IS EXPECTED TO SUPPORT THE NEXT COLD FRONT FORECAST TO EMERGE OFF THE TEXAS AND LOUISIANA COAST BY MONDAY MORNING INTO THE AFTERNOON WITH STRONG NORTHERLY WINDS IN THE RANGE OF 20 TO 25 KT EXPECTED WEST OF THE FRONT. CARIBBEAN SEA... AN UPPER LEVEL TROUGH EXTENDS SOUTHWARD FROM THE SW NORTH ATLC INTO THE CENTRAL CARIBBEAN WITH AXIS FROM OVER HISPANIOLA NEAR 20N70W TO A BASE OVER NORTHERN COLOMBIA AT 20N75W. WEST OF THE UPPER LEVEL TROUGH NORTHWESTERLY DRY AND STABLE FLOW ALOFT DOMINATES WHICH IS PROVIDING MUCH OF THE WESTERN CARIBBEAN W OF 70W WITH FAIR SKIES THIS AFTERNOON. AT THE SURFACE...NE WINDS ARE NOTED IN THE RANGE OF 15 TO 25 KT WITH LOW-LEVEL MOISTURE CONVERGENCE SUPPORTING ISOLATED SHOWERS ALONG THE COAST OF CENTRAL AMERICA...INCLUDING THE GULF OF HONDURAS AND PORTIONS OF THE SW CARIBBEAN W OF 80W. SOME OF THIS MOISTURE AND CLOUDINESS CONTINUES TO ADVECT ONSHORE AND PROVIDE ISOLATED SHOWER ACTIVITY FOR INLAND PORTIONS OF BELIZE...HONDURAS...AND NICARAGUA. FARTHER EAST...THE UPPER LEVEL TROUGHING SUPPORTS A SURFACE TROUGH EXTENDING FROM THE CENTRAL ATLC INTO THE NE CARIBBEAN ALONG 20N63W TO 14N63W. THE LOW-LEVEL CONVERGENCE ASSOCIATED WITH THE SURFACE TROUGH AND AMPLE UPPER LEVEL DIFFLUENCE PROVIDED BY THE MIDDLE TO UPPER LEVEL TROUGH IS GENERATING A BROAD AREA OF WIDELY SCATTERED SHOWERS AND ISOLATED TSTMS E OF A LINE FROM EASTERN PUERTO RICO NEAR 18N66W TO THE GUAJIRA PENINSULA IN NORTHERN COLOMBIA. WITH THE SURFACE TROUGH NEARLY STATIONARY OVER THE PAST 24 HOURS...PRECIPITATION AMOUNTS REPORTED BY GUADELOUPE...TRINIDAD...AND CURACAO WERE IN THE 0.5 TO 1.0 INCH RANGE. BY TUESDAY...THE TROUGHING IS EXPECTED TO WEAKEN AS HIGH PRESSURE CURRENTLY OVER THE SW NORTH ATLC SHIFTS EASTWARD. ATLANTIC OCEAN... AN UPPER LEVEL TROUGH AXIS EXTENDS ALONG 32N62W TO 20N70W AND INTO THE CENTRAL CARIBBEAN SEA. THIS TROUGHING SUPPORTS A SURFACE TROUGH ANALYZED FROM 30N59W TO 18N63W. LOW-LEVEL CONVERGENCE IS MAXIMIZED IN THE VICINITY OF THE SURFACE FEATURE WITH SCATTERED SHOWERS AND ISOLATED TSTMS OCCURRING WITHIN 360 NM EAST...AND 180 NM WEST OF THE AXIS. TO THE WEST OVER THE REMAINDER OF THE SW NORTH ATLC...NE TO E WINDS CONTINUE IN THE RANGE OF 20 TO 30 KT WITH POSSIBLE QUICK-MOVING ISOLATED SHOWERS OCCURRING ACROSS THE BAHAMAS AND NEAR THE EAST COAST OF FLORIDA AND GEORGIA THIS AFTERNOON INTO THE EVENING. FARTHER EAST...AN UPPER LEVEL LOW IS CENTERED NEAR 29N39W AND SUPPORTS A WEAK SURFACE TROUGH AT THE SURFACE ANALYZED FROM 23N40W TO 29N45W. MOST OF THE LOW TO MIDDLE LEVEL MOISTURE CONVERGENCE IS LOCATED TO THE EAST OF THE SURFACE TROUGH WITH WIDELY SCATTERED SHOWERS OCCURRING OVER THE AREA FROM 22N-31N BETWEEN 31W-41W. MUCH OF THIS ACTIVITY IS LIKELY ENHANCED DUE TO THE UPPER LEVEL LOW AND THE ASSOCIATED UPPER LEVEL DIFFLUENCE. OTHERWISE...A RIDGE INFLUENCES THE REMAINDER OF THE EASTERN ATLC ANCHORED BY A 1036 MB HIGH CENTERED OVER THE AZORES NEAR 38N25W. FOR ADDITIONAL INFORMATION PLEASE VISIT HTTP://WWW.HURRICANES.GOV/MARINE $$ HUFFMAN