000 AXNT20 KNHC 041140 TWDAT TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 705 AM EST WED FEB 04 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 1100 UTC. ...THE ITCZ... THE ITCZ IS CENTERED ALONG 5N9W 1N20W ALONG THE EQUATOR BETWEEN 29W-44W AND INTO NE BRAZIL NEAR 1S47W. SCATTERED MODERATE CONVECTION IS WITHIN 100 NM S OF THE AXIS BETWEEN 17W-20W. SIMILAR CONVECTION IS FROM 2S-3N BETWEEN 26W-32W. NUMEROUS MODERATE TO STRONG CONVECTION IS FROM 3S TO THE AXIS W OF 35W INTO NE BRAZIL. ...DISCUSSION... GULF OF MEXICO... A COLD FRONT IS MOVING OFF THE SE CONUS AND INTO THE NRN GULF. AS OF 0900 UTC...THE FRONT ENTERS THE REGION NEAR THE FLORIDA BIG BEND AND STRETCHES WESTWARD ACROSS THE NRN GULF TO TEXAS JUST NORTH OF CORPUS CHRISTI. THE FRONT IS DRY IN NATURE WITH DEW POINT TEMPERATURES DROPPING INTO THE 30S NORTH OF THE FRONT. A 1027 MB SFC HIGH CENTERED NEAR 27N95W ALONG WITH STRONG SUBSIDENCE ALOFT IS MAINTAINING FAIR CONDITIONS ACROSS THE REGION. ONSHORE RETURN FLOW AND LOW-LEVEL CONVERGENCE IN THE SW GULF IS GENERATING CLOUDS AND POSSIBLE SHOWERS ALONG THE COAST OF MEXICO S OF TAMPICO. EXPECT N TO NE WINDS 15 KT TO INCREASE TO 20 KT BEHIND THE FRONT. THE FRONT IS FORECAST TO SINK S ACROSS THE ENTIRE GULF IN THE NEXT 24-36 HOURS WITH HIGH PRESSURE BUILDING IN ITS WAKE. CARIBBEAN SEA... A WEAKENING FRONTAL BOUNDARY REMAINS DRAPED ACROSS THE NW CARIBBEAN FROM EASTERN CUBA NEAR 19N77W TO HONDURAS NEAR 16N84W. NORTHERLY WINDS TO 25 KT ARE OBSERVED IN THE NW CARIBBEAN BEHIND THE FRONT. MULTI-LEVEL CLOUDS WITH POSSIBLE EMBEDDED SHOWERS EXTEND 60 NM BEHIND THE FRONT. EXPECT THIS BOUNDARY TO DISSIPATE LATER TODAY. FRESH TO STRONG TRADE WINDS CONTINUE TO DOMINATE THE REMAINDER OF THE CARIBBEAN USHERING IN ISOLATED LOW-LEVEL SHOWERS. STRONG SUBSIDENCE ASSOCIATED WITH AN UPPER LEVEL RIDGE IS PREVENTING THE DEVELOPMENT OF DEEP CONVECTION. ATLANTIC OCEAN... A DEEP-LAYER TROUGH OVER THE EASTERN CONUS SUPPORTS A COLD FRONT THAT ENTERS THE DISCUSSION AREA NEAR 31N65W AND EXTENDS ACROSS THE EASTERN BAHAMAS TO CUBA NEAR 31N76W. A SFC TROUGH FOLLOWS THE FRONTAL BOUNDARY AND IS ANALYZED FROM 31N68W TO 22N78W. MULTI-LEVEL CLOUDS...SCATTERED SHOWERS AND POSSIBLE THUNDERSTORMS ARE BETWEEN THESE TWO FEATURES. A GALE WARNING IS IN EFFECT N OF 29N WITHIN 120 NM E OF THE COLD FRONT. COLD-AIR STRATOCUMULUS CLOUDS COVER THE W ATLC BEHIND THE SFC TROUGH. THE REMAINDER OF THE CENTRAL AND ERN ATLC IS DOMINATED BY A SURFACE RIDGE ANCHORED ON A 1035 MB HIGH CENTERED NORTH OF THE AREA NEAR 33N41W. $$ WADDINGTON