000 AXNT20 KNHC 011140 TWDAT TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 705 AM EST TUE DEC 01 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 0600 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 1115 UTC. ...ITCZ... THE ITCZ AXIS IS CENTERED ALONG 8N13W 5N30W 4N52W. WIDELY SCATTERED MODERATE CONVECTION IS FROM 3N-10N BETWEEN 8W-29W. ...DISCUSSION... GULF OF MEXICO... AS OF 0900 UTC...A STATIONARY FRONT EXTENDS FROM THE FLORIDA BIG BEND INTO THE NE GULF NEAR 29N83W W-SW ALONG 27N90W TO A 1009 MB LOW NEAR 26N96W THEN SOUTHWARD ALONG 20N95W AND INLAND ACROSS SOUTHERN MEXICO NEAR 18N94W. MOSAIC DOPPLER RADAR IMAGERY SHOWS NUMEROUS SHOWERS AND ISOLATED TSTMS VERY NEAR AND NORTH OF THE FRONTAL BOUNDARY MAINLY COVERING THE GULF W OF 93W AND N OF 24N BETWEEN 85W-93W. THIS SHOWER ACTIVITY FALLS BENEATH AN UPPER LEVEL DIFFLUENT AREA OVER THE NW GULF BETWEEN A VIGOROUS UPPER LEVEL LOW CENTERED OVER N/CENTRAL MEXICO NEAR 31N107W AND AN UPPER LEVEL RIDGE OVER THE NW CARIBBEAN AND SE GULF WITH AXIS EXTENDING FROM CENTRAL AMERICA ALONG 82W TO OVER THE FLORIDA PENINSULA AND W ATLC. TO THE SE OF THE FRONT NORTH OF THE YUCATAN PENINSULA...SCATTERED SHOWERS AND ISOLATED TSTMS ARE OCCURRING FROM 22N-24N BETWEEN 83W-90W. OVER THE NEXT 24-36 HOURS...THE SURFACE LOW WILL CONTINUE TO DEVELOP ALONG THE STATIONARY FRONT IN THE NW GULF WATERS AS THE VIGOROUS UPPER LEVEL LOW CONTINUES SWEEPING EASTWARD OVER NORTHERN MEXICO AND TEXAS. THIS DEVELOPING AREA OF LOW PRESSURE WILL BRING SOUTHERLY WINDS TO GALE FORCE OVER THE NORTHERN GULF WATERS N OF 27N E OF 92W. CARIBBEAN SEA... CENTRAL AMERICA AND THE WESTERN CARIBBEAN SEA W OF 70W ARE UNDER THE INFLUENCE OF AN UPPER LEVEL RIDGE WITH AXIS EXTENDING FROM COSTA RICA ALONG 82W TO WESTERN CUBA AND INTO THE SE GULF OF MEXICO. STRONG SUBSIDENCE ACCOMPANIES THE UPPER LEVEL ANTICYCLONIC CIRCULATION BRINGING MOSTLY TRANQUIL WEATHER AND FAIR SKIES TO MUCH OF THE BASIN. HOWEVER...A FEW ISOLATED SHOWERS ARE BEING USHERED IN ON FRESH TO STRONG TRADEWINDS ACROSS THE EASTERN AND CENTRAL CARIBBEAN. THE STRONGEST OF THESE TRADES ARE LOCATED OFF THE COAST OF NORTHERN COLOMBIA. ATLANTIC OCEAN... AN UPPER LEVEL TROUGH AXIS EXTENDS ALONG 72W IN THE W ATLC N OF 32N AND SUPPORTS A COLD FRONT THAT ENTERS THE DISCUSSION AREA NEAR 32N78W AND EXTENDS TO THE FLORIDA PENINSULA NEAR JACKSONVILLE. SCATTERED SHOWERS AND ISOLATED TSTMS ARE REMAINING MAINLY N OF 32N AND WITHIN 120 NM EAST OF THE FRONT N OF 29N. THE REMAINDER OF THE W ATLC WATERS ARE CONTROLLED BY A WEAK SURFACE RIDGE EXTENDING FROM 30N60W TO THE BAHAMAS AND EASTERN CUBA NEAR 22N77W. FARTHER EAST ACROSS THE CENTRAL ATLC...AN UPPER LEVEL SHORTWAVE TROUGH IS ALONG 53N N OF 20N. THIS UPPER LEVEL FEATURE SUPPORTS A STATIONARY FRONT THAT EXTENDS INTO THE REGION NEAR 32N49W ALONG 30N51W TO 23N52W. LOW-LEVEL CONVERGENCE NEAR THE FRONT IS GENERATING SCATTERED SHOWERS AND TSTMS FROM 22N TO BEYOND 32N BETWEEN 46W-53W. THE REMAINDER OF THE EASTERN ATLC IS UNDER THE INFLUENCE OF A BROAD SURFACE RIDGE ANCHORED BY A 1027 MB HIGH CENTERED SOUTH OF THE AZORES NEAR 34N26W. $$ HUFFMAN