000 AXNT20 KNHC 191051 TWDAT TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 805 AM EDT WED AUG 19 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. ...SPECIAL FEATURES... HURRICANE BILL IS CENTERED NEAR 18.0N 54.9W OR ABOUT 400 NM EAST OF THE LEEWARD ISLANDS MOVING WNW AT 14 KT. ESTIMATED MINIMUM CENTRAL PRESSURE IS 948 MB. MAXIMUM SUSTAINED WIND SPEED IS 115 KT WITH GUSTS TO 140 KT. SEE THE LATEST FORECAST/ADVISORY UNDER AWIPS/WMO HEADERS TCMAT3/WTNT23 KNHC FOR MORE DETAILS. HURRICANE BILL DISPLAYED A WELL DEFINED EYE WITH SCATTERED/NUMEROUS STRONG CONVECTION IS WITHIN 60 NM OF THE CENTER IN ALL QUADRANTS AND SCATTERED MODERATE/ISOLATED STRONG CONVECTION COVERING THE REMAINDER OF THE AREA FROM 15N-22N BETWEEN 51W-57W. ...TROPICAL WAVES... TROPICAL WAVE IS INTRODUCED ALONG 19W S OF 16N MOVING W 10-15 KT. WAVE LOCATION IS AT THE LEADING EDGE OF AN AREA DEEP LAYER MOISTURE MAXIMUM OBSERVED IN TOTAL PRECIPITABLE WATER IMAGERY AND IS CLEARLY DEFINED MAINLY IN THE MID/UPPER LEVELS. CLUSTERS OF SCATTERED MODERATE/ISOLATED STRONG CONVECTION ARE WITHIN 120 NM OF THE WAVE FROM 8N-11N. TROPICAL WAVE REMAINS TILED DUE TO HURRICANE BILL EXTENDING FROM 16N41W TO 8N36W MOVING W 15-20 KT. WAVE CONTINUES TO BE AT THE LEADING EDGE OF AN AREA DEEP LAYER MOISTURE MAXIMUM OBSERVED IN TOTAL PRECIPITABLE WATER IMAGERY. ISOLATED SHOWERS ARE WITHIN 60 NM OF THE AXIS FROM 13N-16N. TROPICAL WAVE IS ALONG 82W S OF 22N MOVING W NEAR 25 KT. THIS WAVE RESULTED FROM THE REMNANTS OF ANA AND IS NOT DISPLAYING THE TYPICAL CHARACTERISTICS OF A TROPICAL WAVE...SUCH AS BEING EMBEDDED WITHIN DEEP LAYERED MOISTURE. IT IS IN AN AREA OF DRY STABLE AIR AND NOT PRODUCING ANY SHOWERS/CONVECTION. ...THE ITCZ... THE ITCZ AXIS IS CENTERED ALONG 13N16W 9N28W 8N46W 11N62W. CLUSTERS OF SCATTERED MODERATE/ISOLATED STRONG CONVECTION ARE INLAND AND WITHIN 90/120 NM ALONG THE COAST OF W AFRICA BETWEEN 8N-16N AND WITHIN 75 NM OF LINE FROM 11N29W TO 13N37W. CLUSTERS OF SCATTERED MODERATE CONVECTION ARE WITHIN 60/75 NM OF 8N BETWEEN 22W-30W. ...DISCUSSION... GULF OF MEXICO... BROAD UPPER RIDGE COVERS THE W GULF WHILE A UPPER LOW IN THE CARIBBEAN EXTENDS AN UPPER TROUGH OVER THE E GULF CONTINUING TO PROVIDE ABUNDANCE OF UPPER LEVEL MOISTURE ACROSS THE ENTIRE AREA. THE SURFACE RIDGE FROM THE W ATLC IS BEGINNING TO BUILD ACROSS THE GULF FROM THE NE TO SW. SCATTERED SHOWERS/ THUNDERSTORMS ARE IN THE BAY OF CAMPECHE S OF 21N W OF 92W TO INLAND OVER MEXICO. SCATTERED SHOWERS/ISOLATED THUNDERSTORMS ARE OVER THE SE GULF WITHIN 75 NM OF LINE FROM 27N85W TO THE NE TIP OF THE YUCATAN PENINSULA. ISOLATED SHOWERS DOT THE REMAINDER OF THE GULF. CARIBBEAN SEA... THE MOST SIGNIFICANT FEATURE FOR THE CARIBBEAN THIS MORNING REMAINS THE UPPER LOW CENTERED NEAR 20N84W COVERING THE NW CARIBBEAN AND EXTENDING AN UPPER TROUGH N OVER THE E GULF OF MEXICO AND SE TO NEAR 12N80W. THIS FEATURE IS GENERATING SCATTERED SHOWERS/ISOLATED THUNDERSTORMS W OF 83W FROM CENTRAL AMERICA TO OVER CUBA AND N OF 20N TO OVER CUBA BETWEEN 80W-83W. UPPER LEVEL DIFFLUENCE COMBINED WITH LOW LEVEL CONVERGENCE ARE GENERATING SCATTERED SHOWERS/ISOLATED THUNDERSTORMS OVER THE SW CARIBBEAN S OF 15N W OF 77W TO INLAND OVER CENTRAL AMERICA. FRESH TO STRONG EASTERLY TRADE WINDS CONTINUE ACROSS THE AREA. DRY STABLE AIR IS ACROSS THE REMAINDER OF THE AREA E OF 80W LIMITING ANY SHOWERS RESULTING IN FAIR CONDITIONS THIS MORNING WITH THE EXCEPTION OF THE FAR NE CARIBBEAN. SCATTERED SHOWERS AND POSSIBLE ISOLATED THUNDERSTORMS ARE MOVING ACROSS THE LEEWARD ISLANDS TO PUERTO RICO BEING PUSHED AHEAD OF HURRICANE BILL AS IT MOVES TO NW OF THE ISLANDS. ATLANTIC OCEAN... THE MAIN FOCUS THIS MORNING FOR THE ATLC IS HURRICANE BILL. THE A SURFACE TROUGH IS OFF THE SE COAST OF FLORIDA JUST W OF THE BAHAMAS FROM 23N79W TO 28N78W GENERATING SCATTERED SHOWERS/ THUNDERSTORMS FROM 23N-27N BETWEEN 76W AND THE SURFACE TROUGH AND SCATTERED SHOWERS/ISOLATED THUNDERSTORMS FROM 24N-26N BETWEEN W OF THE SURFACE TROUGH ACROSS THE S FLORIDA PENINSULA AND THE FLORIDA KEYS. SCATTERED SHOWERS/ISOLATED THUNDERSTORMS AN UPPER RIDGE IS OVER THE FAR W ATLC EXTENDING FROM E CUBA TO JUST W OF BERMUDA BETWEEN A NARROW UPPER TROUGH EXTENDING THROUGH 32N75W TO 28N78W AND AN UPPER LOW TO THE E OF BERMUDA NEAR 32N60W. DIFFLUENCE ALOFT IS GENERATING SCATTERED SHOWERS/ ISOLATED THUNDERSTORMS FROM 28N-30N BETWEEN 69W-71W. OTHERWISE THE ATLC BASIN IS DOMINATED BY A SURFACE RIDGE OVER THE W ATLC ANCHORED BY A 1021 MB HIGH BETWEEN BERMUDA AND NORTH CAROLINA COAST AND BY A 1022 MB HIGH NEAR 30N31W IN THE E WITH A WEAKNESS OVER THE CENTRAL ATLC COMPLIMENTS OF HURRICANE BILL. $$ WALLACE