000 AXNT20 KNHC 132352 TWDAT TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 805 PM EDT SAT MAY 13 2006 TROPICAL WEATHER DISCUSSION FOR NORTH AMERICA...CENTRAL AMERICA...THE GULF OF MEXICO...THE CARIBBEAN SEA...NORTHEASTERN SECTIONS OF SOUTH AMERICA...AND THE 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 1800 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 2315 UTC. ...TROPICAL WAVES... TROPICAL WAVE ALONG 44W S OF 9N MOVING W 10 KT. WAVE HAS BEEN MOVING SLOWLY DUE TO WEAK RIDGING TO THE N. LOW-LEVEL CYCLONIC FEATURE TO THE W DOES NOT APPEAR TO BE DIRECTLY ASSOCIATED WITH THE WAVE. WIDELY SCATTERED MODERATE CONVECTION IS FROM 4.5N-8.5N BETWEEN 40W-45W. THE GFS SUGGESTS THAT MOISTURE FROM THE WAVE COULD IMPACT THE WINDWARD ISLANDS LATE TUE INTO WED. ...ITCZ... ITCZ AXIS ALONG 7N12W 4N20W 2N30W 4N40W 4N51W. SCATTERED MODERATE CONVECTION BETWEEN 8W-14W FROM 2N-7N. WIDELY SCATTERED MODERATE CONVECTION N OF 2N BETWEEN 3W-8W AND S OF 3.5N BETWEEN 14W-20W. CLUSTERS OF MODERATE CONVECTION ARE WITHIN 90 NM OF 3N34W. ...DISCUSSION... GULF OF MEXICO... MUCH DEEPER THAN AVERAGE NEARLY STATIONARY DEEP LAYERED CYCLONIC VORTEX SITTING OVER THE GREAT LAKES HAS A LONGWAVE UPPER LEVEL TROUGH THAT DIGS SWWD ACROSS THE GULF. UPPER LEVEL CONFLUENT FLOW IS GENERATING STRONG SUBSIDENCE ACROSS THE AREA N OF 24N...SINKING SEWARD. UPPER LEVEL CLOUDINESS IS THINNING S OF THE TROUGHW S OF 25N. AT THE SFC...A 1016 MB HIGH IS CENTERED 150 NM S OF THE AL COAST NEAR 28N87.5W. CONTINENTAL AIR CONTROLS THE REGION WITH MOSTLY CLEAR SKIES UNDER STRONG SUBSIDENCE. WINDS ARE FAIRLY LIGHT...GENERALLY FROM THE N E OF THE HIGH...TRANSITIONING TO SLY IN THE W GULF. SMOKE IS VISIBLE ON LATE DAY VISIBLE SATELLITE PICTURES S OF 24N WITH PLENTY OF MILKY PLUMES SEEN. WEAK SFC HIGH PRES WILL SHIFT TO THE E OF THE AREA LATE TOMORROW AS A COLD FRONT ENTERS THE NW GULF. THE LATEST GFS RUN INDICATES THAT THIS FRONT WILL BE FAIRLY STRONG AND MAY CLEAR THE ENTIRE AREA BY EARLY WED. A GOOD CHANCE OF RAIN IS LIKELY AS THE FRONT APPROACHES WHICH COULD AID DROUGHT-PARCHED AREAS OF THE SE USA. CARIBBEAN SEA... BROAD UPPER LEVEL RIDGING COVERS THE AREA GENERATING DRY/STABLE AIR ALOFT S OF 17N KEEPING MUCH OF THE REGION SHOWER FREE. THE SOUTHEASTERN PERIPHERY OF RIDGE HAS PROMPTED SCATTERED SHOWERS/ISOLATED TSTMS INLAND COLOMBIA AND PANAMA. TYPICAL LOW-LEVEL CYCLONIC WINDS IN THE SW CARIBBEAN HAS SHIFTED IN THE CENTRAL CARIBBEAN WITH TROUGHING NOTED S OF THE DOMINICAN REPUBLIC ALONG 70W AND RATHER RELAXED TRADES IN THE W/CENTRAL CARIBBEAN. UPPER LEVEL MOISTURE IS STREAMING NEWARD ACROSS THE NW CARIBBEAN FROM A CONVECTIVE AREA OF LOW PRES IN THE EPAC EMBEDDED WITHIN THE ITCZ. SCATTERED SHOWERS/ISOLATED TSTMS ARE MAINLY ACROSS THE W COAST OF CENTRAL AMERICA. AT THE SFC...THE TAIL END OF A W ATLC COLD FRONT STRETCHES ACROSS W-CENTRAL CUBA BUT IS DISSIPATING IN THE CARIBBEAN. A BROAD SFC RIDGE WILL BECOME BETTER ESTABLISHED NE OF THE AREA EARLY NEXT WEEK INCREASING THE TRADES ESPECIALLY IN THE E AND CENTRAL CARIBBEAN. ATLANTIC OCEAN... A LARGE DEEP-LAYERED LOW OVER THE GREAT LAKES IS SUPPORTING A SFC COLD FRONT WHICH ENTERS THE AREA ALONG 31N69W 25N75W TO W-CENTRAL CUBA. MULTILAYERED CLOUDS AND ISOLATED SHOWERS STRETCH WITHIN 180 NM TO THE E OF THE FRONT N OF 25N. ZONAL FLOW IS E OF THE UPPER TROUGH FROM 65W TO 50W WHERE A BROAD DEEP LAYERED TROUGH COVERS THE CENTRAL/EAST ATLC N OF 22N FROM 35W-50W. TROUGHING DIPS SOUTHWARD INTO THE DEEP TROPICS AONG 22N49W TO 12N60W. ASSOCIATED COLD FRONT ENTERS THE AREA ALONG 31N30W 27N39W THEN AS A DISSIPATING STATIONARY FRONT TO 31N51W. A SFC TROUGH IS 150 NM TO THE E OF THE FRONT ALONG 31N27W 21N40W. ISOLATED SHOWERS ARE WITHIN 60 NM SE OF THE TROUGH AXIS. AT THE SFC...A 1019 MB HIGH IS LOCATED NEAR 25N51W AND IN THE EAST ATLC...A 1029 MB HIGH IS CENTERED NEAR 27N23W WITH SFC RIDGING STRETCHING SWWARD TO 16N36W. FAIR WEATHER EXISTS UNDER THE INFLUENCE OF THE SFC RIDGE WITH NEAR AVERAGE TRADES. IN THE TROPICAL ATLC...A BROAD UPPER LEVEL HIGH IS CENTERED NEAR 13N30W GENERATING STRONG SUBSIDENCE FROM 6N-15N E OF 34W. A TROPICAL JET ORIGINATES ON THE W PERIPHERY OF THE UPPER HIGH AND RACES TO THE NE ALONG 12N54W 24N35W 31N23W. UPPER RIDGING IS MORE ENHANCED THAN AVERAGE IN THE TROPICAL E ATLC.. TYPICAL OF THE PAST COUPLE OF MONTHS. $$ BLAKE