000 AXNT20 KNHC 020601 TWDAT TROPICAL WEATHER DISCUSSION NWS NATIONAL HURRICANE CENTER MIAMI FL 105 AM EST FRI MAR 02 2012 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 0000 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 0515 UTC. ...THE ITCZ/THE MONSOON TROUGH... THE MONSOON TROUGH IS NON-EXISTENT IN THE ATLANTIC OCEAN OFF THE COAST OF AFRICA. THE ITCZ IS ALONG 4N12W 3N13W 3N16W...CROSSING THE EQUATOR ALONG 16W...1S31W TO THE EQUATOR BETWEEN 35W AND 41W...CONTINUING INTO NORTHEASTERN COASTAL BRAZIL NEAR 2S46W. ISOLATED MODERATE CONVECTIVE PRECIPITATION IS TO THE SOUTH OF 4N TO THE EAST OF 50W. ...DISCUSSION... THE GULF OF MEXICO... BROAD UPPER LEVEL ANTICYCLONIC WIND FLOW SPANS THE AREA. A SURFACE RIDGE PASSES THROUGH 26N72W IN THE ATLANTIC OCEAN TO SOUTH FLORIDA...INTO THE CENTRAL GULF OF MEXICO...TOWARD THE LOWER TEXAS GULF COAST. FROM THE ATLANTIC OCEAN INTO THE CARIBBEAN SEA... AND THE REST OF THE CARIBBEAN SEA... AN UPPER LEVEL TROUGH EXTENDS FROM 22N62W IN THE ATLANTIC OCEAN...THROUGH THE MONA PASSAGE...INTO THE CENTRAL CARIBBEAN SEA...BEYOND COSTA RICA INTO THE EASTERN PACIFIC OCEAN. RAINSHOWERS ARE POSSIBLE FROM 18N TO 21N BETWEEN 63W AND 65W... TO THE NORTH OF ANGUILLA...THE ANEGADA PASSAGE...AND THE VIRGIN ISLANDS. A SURFACE TROUGH IS ALONG 14N64W 12N63W 9N62W...FROM THE WATERS INTO NORTHEASTERN VENEZUELA. SCATTERED MODERATE CONVECTIVE PRECIPITATION IS FROM 11N TO 13N BETWEEN 60W AND 63W. THE REST OF THE ATLANTIC OCEAN... A SURFACE RIDGE EXTENDS FROM A 1029 MB HIGH PRESSURE CENTER THAT IS NEAR 33N18W...TO 29N31W 27N43W 27N58W 26N72W...AND BEYOND SOUTH FLORIDA INTO THE CENTRAL GULF OF MEXICO. MIDDLE LEVEL TO UPPER LEVEL TROUGH THAT IS TO THE NORTH OF 33N SUPPORTS A COLD FRONT THAT PASSES THROUGH 32N42W TO 31N44W. A DISSIPATING COLD FRONT CONTINUES FROM 31N44W TO 29N49W AND 31N62W. A SURFACE TROUGH PASSES THROUGH 32N36W TO 27N44W. AN UPPER LEVEL TROUGH REACHES ITS BASE NEAR 33N11W. THIS TROUGH SUPPORTS A DISSIPATING COLD FRONT THAT PASSES THROUGH 31N14W TO 27N24W. FOR ADDITIONAL INFORMATION PLEASE VISIT HTTP://WWW.HURRICANES.GOV/MARINE $$ MT