000 AXNT20 KNHC 081041 TWDAT TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 805 AM EDT SAT AUG 08 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. ...TROPICAL WAVES... TROPICAL WAVE EXTENDS ALONG 9N21W JUST W OF THE CAPE VERDE ISLANDS TO 18N29W MOVING W NEAR 15 KT. WAVE REMAINS EMBEDDED WITH A MOISTURE MAXIMUM OBSERVED IN TOTAL PRECIPITABLE WATER IMAGERY. THERE IS NO DEEP CONVECTION ASSOCIATED WITH THE WAVE BUT ISOLATED SHOWERS ARE WITHIN 120 NM EITHER SIDE OF THE WAVE AXIS FROM 13N-16N. TROPICAL WAVE IS ALONG 40W/41W S OF 16N MOVING W NEAR 15 KT. WAVE IS MOVING THROUGH AN AREA OF DRY STABLE AIR AND THE LOCATION IS BASED ON CONTINUITY WITH NO ASSOCIATED SHOWERS OR DEEP CONVECTION. TROPICAL WAVE IS ALONG 57W/58W S OF 15N MOVING W NEAR 15 KT. WAVE REMAINS IN AN AREA BENEATH AN UPPER RIDGE THUS MASKING THE WAVE SIGNATURE AND THE CONVECTION MAY BE ASSOCIATED MORE WITH THE ITCZ THAN THE WAVE ITSELF. SCATTERED MODERATE/ISOLATED STRONG CONVECTION IS WITHIN 60/75 NM OF LINE FROM 13N54W TO 11N59W. TROPICAL WAVE IS ALONG 75W S OF 19N MOVING W NEAR 15 KT. WAVE IS NOW ALONG THE TRAILING EDGE OF A MOISTURE MAXIMUM OBSERVED IN TOTAL PRECIPITABLE WATER IMAGERY. SCATTERED SHOWERS/ISOLATED THUNDERSTORMS ARE W OF THE WAVE FROM 14N-16N BETWEEN 76W-79W. TROPICAL WAVE IS ALONG 93W/94W S OF 21N MOVING W 15-20 KT. WAVE REMAINS WITHIN A BROAD AREA OF DEEP LAYER MOISTURE AS NOTED ON TOTAL PRECIPITABLE WATER IMAGERY THAT COVERS THE GULF OF MEXICO AND INTO THE E PACIFIC REGION. SCATTERED SHOWERS/ISOLATED THUNDERSTORMS ARE OVER THE BAY OF CAMPECHE S OF 21N TO OVER MEXICO BETWEEN THE WAVE AXIS AND 97W WITH ISOLATED SHOWERS S OF 24N BETWEEN 89W-93W INCLUDING THE YUCATAN PENINSULA. ...ITCZ... THE ITCZ AXIS IS CENTERED ALONG 13N15W 9N31W 13N50W 10N63W. A NEAR STATIONARY SURFACE TROUGH IS EMBEDDED WITHIN THE ITCZ EXTENDING FROM 15N46W TO 8N51W WITH SCATTERED MODERATE/ISOLATED STRONG CONVECTION W OF THE TROUGH AXIS WITHIN 120 NM OF LINE FROM 15N49W TO 11N53W. SCATTERED MODERATE/ISOLATED STRONG CONVECTION HAS MOVED OFF W AFRICA WITHIN 75/90 NM OF LINE FROM 12N20W TO THE COAST NEAR 10N14W. SCATTERED CLUSTERS OF SCATTERED MODERATE CONVECTION ARE WITHIN 75 NM OF 10N BETWEEN 43W-47W. ...DISCUSSION... GULF OF MEXICO... AN UPPER LEVEL TROUGH EXTENDS ACROSS THE GULF OF MEXICO FROM AN UPPER LOW OVER MOBILE ALABAMA THROUGH 25N95W TO A SECOND UPPER LOW CENTERED OVER E/CENTRAL MEXICO NEAR 22N99W. A SURFACE TROUGH EXTENDS JUST TO THE SE OF THIS UPPER TROUGH FROM NEAR JACKSONVILLE FLORIDA ALONG 28N86W TO 25N90W WITH CLUSTERS OF SCATTERED SHOWERS/ISOLATED THUNDERSTORMS FROM 25N-30N BETWEEN 83W-90W. ISOLATED SHOWERS/THUNDERSTORMS DOT THE REMAINDER OF THE W GULF. A BROAD UPPER RIDGE EXTENDS FROM THE OVER THE YUCATAN PENINSULA OVER THE REMAINDER OF THE E GULF. CARIBBEAN SEA... AN UPPER RIDGE OVER THE YUCATAN PENINSULA INTO THE E GULF OF MEXICO COVERS THE W CARIBBEAN...WITH AN UPPER TROUGH OVER THE CENTRAL CARIBBEAN...AND A SECOND UPPER RIDGE OVER THE E CARIBBEAN. THE UPPER LEVEL DIFFLUENCE OVER THE W/CENTRAL CARIBBEAN IS GENERATING SCATTERED SHOWERS/ISOLATED THUNDERSTORMS FROM S OF 12N TO OVER PANAMA BETWEEN 77W-81W AND S OF 17N W OF 81W TO INLAND OVER CENTRAL AMERICA. THE CARIBBEAN E OF 75W IS DOMINATED BY DRY STABLE AIR LIMITING SHOWER ACTIVITY. FRESH TO STRONG TRADE WINDS CONTINUE ACROSS MUCH OF THE E AND CENTRAL CARIBBEAN. ATLANTIC OCEAN... AN UPPER RIDGE IS OVER THE W ATLC ANCHORED OVER THE N BAHAMA ISLANDS WITH A NARROW UPPER TROUGH TO THE E EXTENDING THROUGH 32N63W THROUGH THE WINDWARD PASSAGE AND OVER THE CENTRAL CARIBBEAN. THIS COMBINATION IS PROVIDING UPPER LEVEL DIFFLUENCE TO GENERATE CLUSTERS OF SCATTERED SHOWERS/ISOLATED THUNDERSTORMS WITHIN 75/90 NM OF LINE FROM THE BAHAMAS NEAR 24N76W TO BEYOND 32N68W. A SURFACE TROUGH IS BENEATH THE UPPER RIDGE EXTENDING FROM 29N73W TO OVER THE BAHAMAS NEAR 25N77W BUT IS NOT GENERATING ANY SIGNIFICANT WEATHER. A LARGE UPPER LOW IS IN THE CENTRAL ATLC NEAR 28N46W WITH A SURFACE TROUGH EXTENDING 31N47W TO 25N44W. SCATTERED SHOWERS AND POSSIBLE ISOLATED THUNDERSTORMS ARE ALONG THE N PERIPHERY OF THE UPPER LOW WITHIN 75 NM OF LINE FROM 32N45W TO 27N52W AND ISOLATED SHOWERS WITHIN 90 NM EITHER SIDE OF THE SURFACE TROUGH. THE REMAINDER OF THE ATLC REMAINS TRANQUIL THIS MORNING WITH A BROAD AREA OF SAHARAN DUST COVERING THE AREA E OF 42W AND FROM 60W-72W. $$ WALLACE