000 AXNT20 KNHC 041041 TWDAT TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 805 AM EDT MON MAY 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 1015 UTC. ...THE ITCZ... THE ITCZ AXIS IS ALONG 6N10W 1N20W CROSSING THE EQUATOR NEAR 23W AND CONTINUING ALONG 1S30W 1S40W AND INTO NE BRAZIL NEAR 2S44W. SCATTERED MODERATE/ISOLATED STRONG CONVECTION IS WITHIN 150 NM N OF THE AXIS BETWEEN 14W-25W. SIMILAR CONVECTION IS LOCATED FROM 3S TO 3N BETWEEN 30W-36W. ...DISCUSSION... GULF OF MEXICO... THE COMBINATION OF BROAD SURFACE LOW PRESSURE ACROSS THE MEXICAN PLATEAU AND A SURFACE RIDGE EXTENDING FROM THE W ATLC ACROSS THE FLORIDA PENINSULA INTO THE NRN GULF IS PRODUCING SE WINDS FROM 10 TO 20 KT. NO ORGANIZED AREAS OF DEEP CONVECTION ARE OCCURRING OVER THE GULF...HOWEVER A MIDDLE TO UPPER LEVEL SHORTWAVE TROUGH IS MOVING ACROSS THE SE CONUS AND IS SUPPORTING A STATIONARY FRONT ACROSS SRN ALABAMA...MISSISSIPPI...AND LOUISIANA THAT CONTINUES TO PRODUCE SCATTERED SHOWERS AND TSTMS INLAND OVER THE SE CONUS. A COLD FRONT IS ALSO POSITIONED ALONG THE IMMEDIATE TEXAS GULF COAST. THIS FRONT IS FORECAST TO BRUSH THE NW GULF WATERS OVER THE NEXT 24 HOURS BEFORE WEAKENING SLIGHTLY AND LIFTING NORTHWARD AS A STATIONARY BOUNDARY. UPPER LEVEL WINDS WILL CONTINUE TO TRANSITION TO MORE OVERALL ZONAL FLOW AS THE SHORTWAVE TROUGH LIFTS OFF TO THE NE. ONLY A FEW BANDS OF CIRRUS CLOUDS STRETCH ACROSS THE NE GULF ON DIFFLUENT FLOW LOCATED ACROSS THE ERN GULF AND FLORIDA. CARIBBEAN SEA... FRESH TRADEWINDS REMAIN ACROSS THE CARIBBEAN AS THE ANALYZED PRESSURE FIELD CONTINUES TO EXHIBIT A RELATIVELY RELAXED GRADIENT. A SURFACE TROUGH EXISTS IN THE ERN CARIBBEAN EXTENDING FROM THE U.S. VIRGIN ISLANDS SWD ALONG 65W TO THE NE COAST OF VENEZUELA. SCATTERED SHOWERS ARE AFFECTING THE LESSER ANTILLES AND NE CARIBBEAN MAINLY N OF A SAINT LUCIA TO WRN PUERTO RICO LINE...AS OBSERVED FROM THE GUADELOUPE...MARTINIQUE AND PUERTO RICO RADARS. ELSEWHERE...AN UPPER LEVEL HIGH CENTERED OVER NRN COLOMBIA EXTENDS RIDGING TO THE NW ACROSS CENTRAL AMERICA AS FAR N AS BELIZE AND GUATEMALA. UPPER DIFFLUENCE IS GENERATING A FEW ISOLATED SHOWERS AND TSTMS ACROSS THE SW CARIBBEAN S OF 11N WITH MORE SCATTERED ACTIVITY INLAND ACROSS NRN SOUTH AMERICA. DEBRIS MOISTURE FROM THE CONVECTION OVER COLOMBIA AND VENEZUELA...IN THE FORM OF SCATTERED CIRRUS CLOUDS...IS SPREADING NE ACROSS MUCH OF THE CARIBBEAN. ATLANTIC OCEAN... THE ATLANTIC IS DOMINATED BY A SURFACE HIGH PRESSURE CENTERED WELL NORTH OF THE DISCUSSION AREA NEAR 46N21W WITH RIDGING EXTENDING WEST-SOUTHWESTWARD TO 34N54W AND TO THE FLORIDA PENINSULA. TWO SMALLER SCALE FEATURES ARE OF INTEREST WHICH ARE EMBEDDED WEAKNESSES WITHIN THE SURFACE RIDGE. THE FIRST IS A SURFACE TROUGH NE OF PUERTO RICO ALONG 69W FROM ROUGHLY 21N TO 29N. THIS TROUGH HAS BEEN PROGRESSING W-NW WITH A MIDDLE TO UPPER LEVEL LOW OBSERVED ON WATER VAPOR IMAGERY W OF THE SURFACE TROUGH CENTERED NEAR 28N70W. SCATTERED SHOWERS AND ISOLATED TSTMS ARE PRESENT WITHIN 90 NM OF A LINE FROM 21N62W TO 28N69W. THE SURFACE WINDS ARE ENHANCED E OF THE TROUGH AXIS WITH E TO SE WINDS OF UP TO 25 KT. THE SECOND FEATURE IS A SURFACE TROUGH EXTENDING FROM 25N38W TO BEYOND 32N43W. SCATTERED SHOWERS ARE OCCURRING E OF THE SURFACE TROUGH FROM 28N-34N BETWEEN 35W-41W. A BROAD UPPER LOW CENTERED NEAR 31N38W ASSOCIATED WITH THE SURFACE TROUGH DOMINATES THE UPPER LEVEL WINDS OVER MOST OF THE CENTRAL ATLC WITH CYCLONICALLY TURNING WINDS OBSERVED AS FAR S AS 10N. FINALLY...THERE IS AN ENHANCEMENT OF NELY SURFACE WINDS OF 20-25 KT NORTHEAST OF THE CAPE VERDE ISLANDS TO THE WEST COAST OF MAURITANIA AND SENEGAL. OVER THE NEXT FEW DAYS...THE SURFACE TROUGH N OF PUERTO RICO IS FORECAST TO CONTINUE MOVING NORTHWESTWARD...WHILE THE TROUGH IN THE CENTRAL ATLANTIC SHOULD GRADUALLY FILL. $$ HUFFMAN