000 AXNT20 KNHC 061711 TWDAT TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 205 PM EDT WED MAY 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 1645 UTC. ...THE ITCZ... THE ITCZ AXIS IS ALONG 7N7W 3N16W 2N25W CROSSING THE EQUATOR NEAR 32W AND CONTINUING S OF THE EQUATOR ALONG 1S37W INTO NE BRAZIL NEAR 1S47W. SCATTERED MODERATE/STRONG CONVECTION IS FROM THE COAST OF SW AFRICA TO THE EQUATOR BETWEEN 2W-10W. SCATTERED MODERATE WITH EMBEDDED CLUSTERS OF ISOLATED STRONG CONVECTION COVERS THE AREA FROM THE EQUATOR TO 9N BETWEEN 10W-20W. CLUSTERS OF SCATTERED MODERATE CONVECTION ARE ELSEWHERE FROM THE EQUATOR TO 4N BETWEEN 23W-40W. ...DISCUSSION... GULF OF MEXICO... THE GULF REMAINS RATHER TRANQUIL THIS AFTERNOON AS SE TO S SURFACE FLOW DOMINATES ACROSS THE ENTIRE REGION S OF A FRONTAL BOUNDARY LOCATED WELL NORTH OF THE GULF COAST ACROSS PORTIONS OF THE SE U.S. AND E TEXAS. AN UPPER LEVEL SHORTWAVE TROUGH MOVING OVER THE LOWER MISSISSIPPI VALLEY CONTINUES TO SUPPORT THE FRONTAL BOUNDARY WITH A PUSH OF MID/HIGH LEVEL CLOUDINESS STREAMING OVER THE FAR NW GULF WATERS OFF THE COAST OF LOUISIANA AND TEXAS. THE FRONTAL BOUNDARY IS EXPECTED TO REMAIN WELL NORTH OF THE GULF COAST AS A SURFACE RIDGE ANCHORED IN THE W ATLC HOLDS IN PLACE ACROSS THE FLORIDA PENINSULA AND GULF WATERS THROUGH THE WEEKEND. LITTLE CHANGE IS EXPECTED IN THE OVERALL PATTERN DURING THE NEXT 24-48 HOURS WITH FAIR WEATHER CONDITIONS PREVAILING THROUGH EARLY SUNDAY. CARIBBEAN SEA... A BROAD UPPER LEVEL RIDGE DOMINATES THE W CARIBBEAN ANCHORED OVER NICARAGUA WHICH IS ADVECTING TROPICAL MOISTURE INTO THE GULF OF HONDURAS AND W CARIBBEAN TO 76W. THIS MOISTURE IS RESULTING IN HIGH DEBRIS CLOUDS FROM 16N-20N BETWEEN 76W-87W INCLUDING JAMAICA. ALOFT ACROSS THE E CARIBBEAN...UPPER LEVEL TROUGH EXTENDS FROM THE W ATLC ACROSS HISPANIOLA TO NEAR 15N68W WITH A WEAK SURFACE TROUGH EXTENDING ACROSS HISPANIOLA NEAR 20N71W TO 15N69W. THE EASTERLY TRADES ALONG WITH THE UPPER LEVEL TROUGHING IS GENERATING SCATTERED SHOWERS AND ISOLATED THUNDERSTORMS N OF 15N E OF THE SURFACE TROUGH TO OVER THE LEEWARD/VIRGIN ISLANDS AND PUERTO RICO. ELSEWHERE...LIGHT TO MODERATE TRADE WINDS COVER THE CARIBBEAN PRIMARILY DUE TO A RELAXED PRESSURE GRADIENT LEAVING THE REMAINDER OF THE CARIBBEAN WITH POSSIBLE ISOLATED LOW LEVEL SHOWER ACTIVITY MOVING WESTWARD IN CONVERGENT SURFACE FLOW ACROSS THE BASIN. THIS FLOW IS ALSO BANKING LOW LEVEL CLOUDS WITH SCATTERED SHOWERS AND POSSIBLE ISOLATED THUNDERSTORMS INLAND AND WITHIN 90 NM ALONG THE COAST OF CENTRAL AMERICA S OF 13N W OF 81W. ATLANTIC OCEAN... THE W ATLC CONTINUES TO BE DOMINATED BY A SURFACE HIGH PRESSURE RIDGE ANCHORED BY A 1033 MB HIGH LOCATED N OF THE DISCUSSION AREA NEAR 36N54W. A WEAKNESS IN THE SURFACE RIDGE...ANALYZED AS A SURFACE TROUGH EXTENDS FROM 27N72W OVER THE EASTERN MOST TURKS AND CAICOS INTO THE CARIBBEAN ACROSS HISPANIOLA NEAR 20N71W. THIS SURFACE FEATURE IS CONTINUING TO LOSE UPPER LEVEL SUPPORT FROM A BROAD UPPER TROUGH THAT EXTENDS THROUGH 32N74W S TO 26N74W INTO THE NE CARIBBEAN ACROSS HISPANIOLA AND IS EMBEDDED WITHIN A SUBSIDENT DRY AIRMASS BUT IS GENERATING AN AREA OF UPPER LEVEL DIFFLUENCE FURTHER TO THE E WHICH IS PRODUCING SCATTERED SHOWERS AND POSSIBLE ISOLATED THUNDERSTORMS WITHIN 150/200 NM OF A LINE FROM THE U.S. VIRGIN ISLANDS NNW TO 32N69W. SCATTERED SHOWERS ARE FARTHER TO THE SE ACROSS THE LESSER ANTILLES AND TROPICAL ATLC FROM 14N-20N BETWEEN 57W-68W. THE SECOND WEAKNESS IN THE ATLC SURFACE RIDGE EXTENDS OVER THE E/CENTRAL ATLC AS AN ELONGATED NE/SW UPPER LEVEL LOW CENTERED NEAR 29N35W PROVIDING SUPPORT FOR A SURFACE TROUGH THAT EXTENDS FROM 32N35W SW TO 26N42W GENERATING SCATTERED SHOWERS AND POSSIBLE ISOLATED THUNDERSTORMS FROM 28N-32N BETWEEN 32W AND THE SURFACE TROUGH. THE REMAINDER OF THE E AND CENTRAL ATLC IS UNDER FAIR WEATHER CONDITIONS. $$ WALLACE