000 AXNT20 KNHC 200514 TWDAT TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 105 AM EST FRI FEB 20 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 0000 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 0445 UTC. ...THE ITCZ... THE ITCZ AXIS IS CENTERED ALONG 5N9W 3N15W CROSSING THE EQUATOR NEAR 19W THEN ALONG 2S BETWEEN 22W-36W AND INTO NE BRAZIL NEAR 4S40W. SCATTERED MODERATE TO STRONG CONVECTION IS WITHIN 130 NM N OF THE AXIS BETWEEN 14W-20W. SCATTERED MODERATE CONVECTION IS S OF THE AXIS FROM THE EQUATOR TO 4N BETWEEN 8W-13W. ...DISCUSSION... GULF OF MEXICO... A DEEP-LAYER TROUGH OVER THE EASTERN SEABOARD EXTENDS A COLD FRONT THROUGH THE W ATLANTIC ACROSS THE FLORIDA PENINSULA AND INTO THE GULF OF MEXICO. AS OF 0300 UTC...THE FRONT ENTERS THE GULF NEAR NAPLES AND CONTINUES ALONG 24N85W TO 23N94W WHERE IT DIPS SOUTH INTO THE WESTERN BAY OF CAMPECHE AS A STATIONARY FRONT AND CROSSES INLAND OVER MEXICO NEAR VERACRUZ. SCATTERED SHOWERS AND ISOLATED THUNDERSTORMS ARE OBSERVED ALONG THE BOUNDARY...PARTICULARLY W OF 86W. STRONG N TO NE WINDS OF 20-25 KT CONTINUE TO ADVECT A COOLER AND DRIER AIRMASS ACROSS THE GULF IN THE WAKE OF THE FRONT. THE FRONT IS EXPECTED TO MOVE SE OF THE REGION FRI NIGHT WITH SFC HIGH PRESSURE SHIFTING EAST ACROSS THE GULF THROUGH SAT. AHEAD OF THE FRONT...FAIR WEATHER CONDITIONS ARE OBSERVED ACROSS THE SE GULF AND THE YUCATAN PENINSULA UNDER NEAR ZONAL FLOW AND MODERATE SUBSIDENCE ALOFT. CARIBBEAN SEA... HIGH PRESSURE OVER THE CENTRAL ATLANTIC IS MAINTAINING FRESH TO STRONG TRADE WIND FLOW ACROSS THE CARIBBEAN. THE STRONGEST WINDS...UP TO 30 KT...ARE OBSERVED ALONG THE COAST OF COLOMBIA. ISOLATED SHOWERS...REMNANTS OF A FRONTAL BOUNDARY...ARE MOVING ACROSS PUERTO RICO AND THE MONA PASSAGE. ADDITIONAL ISOLATED TRADE WIND SHOWERS ARE TRAVERSING THE CARIBBEAN MAINLY E OF 67W. CONVECTION IN THE CARIBBEAN REMAINS SHALLOW DUE TO STRONG SUBSIDENCE AROUND AN UPPER-LEVEL RIDGE THAT EXTENDS FROM SOUTH AMERICA TO THE NW CARIBBEAN. ATLANTIC OCEAN... A COLD FRONT ASSOCIATED WITH A DEEP-LAYER TROUGH OVER THE EASTERN SEABOARD STRETCHES ACROSS THE W ATLC. AS OF 0300 UTC...THE FRONT ENTERS THE DISCUSSION AREA NEAR 31N73W... STRETCHES SOUTHWESTWARD ACROSS FLORIDA NEAR WEST PALM BEACH AND CONTINUES INTO THE GULF OF MEXICO. SCATTERED SHOWERS AND ISOLATED THUNDERSTORMS ARE OBSERVED WITHIN 50 NM OF THE FRONT. THE STRONG PRESSURE GRADIENT ACROSS THE FRONT IS GENERATING SOUTHWESTERLY GALE FORCE WINDS AHEAD OF THE FRONT TO 66W. EAST OF THE FRONT...FAIR WEATHER AND STRATOCUMULUS CLOUDS SURROUND A 1027 MB SFC HIGH CENTERED NEAR 32N50W. A STRONG LOW-PRESSURE SYSTEM WELL NORTH OF THE DISCUSSION AREA EXTENDS A FRONTAL BOUNDARY INTO THE CENTRAL ATLC. THE STATIONARY FRONT ENTERS THE REGION NEAR 31N37W AND CONTINUES TO NEAR 25N44W WHERE IT BECOMES DIFFUSE TO NEAR 19N59W. SURFACE CONFLUENCE NEAR THIS BOUNDARY IS SUPPORTING INCREASED CLOUDINESS AND ISOLATED SHOWERS WITHIN 60 NM EITHER SIDE OF THE FRONT. FAIR WEATHER ASSOCIATED WITH A SFC RIDGE COVERS THE E ATLC E OF 35W. IN THE TROPICS... DEEP-LAYER DRY AIR EMBEDDED WITHIN AN UPPER TROUGH IS SUPPRESSING CONVECTION OVER THE WRN HALF OF THE ITCZ. UPPER LEVEL DIVERGENCE E OF THIS TROUGH IS ENHANCING THE CONVECTION OVER THE ERN HALF OF THE ITCZ. $$ WADDINGTON