000 AXNT20 KNHC 251814 TWDAT TROPICAL WEATHER DISCUSSION...COR NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 105 PM EST SAT NOV 25 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 1200 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 1715 UTC. ...THE ITCZ... ITCZ AXIS IS CENTERED ALONG 9N13W 7N20W 7N30W 8N50W 9N61W. ISOLATED MODERATE CONVECTION IS OFF THE COAST OF W AFRICA FROM 5N-11N BETWEEN 15W-24W. SCATTERED MODERATE TO ISOLATED STRONG CONVECTION IS FROM 4N-10N BETWEEN 32W-43W...AND FROM 6N-13N BETWEEN 43W-49W. WIDELY SCATTERED MODERATE CONVECTION IS E OF THE WINDWARD ISLANDS FROM 11N-14N BETWEEN 55W-59W. ...DISCUSSION... THE GULF OF MEXICO... A 1027 MB HIGH IS CENTERED OVER NORTH CAROLINA NEAR 36N82W. A RIDGE AXIS EXTENDS SW TO W GULF OF MEXICO NEAR 26N97W. 10-15 KT ELY SURFACE WINDS ARE OVER THE GULF OF MEXICO. SCATTERED LOW CLOUDS DOTS THE GULF. IN THE UPPER LEVELS...WLY ZONAL FLOW WITH STRONG SUBSIDENCE DOMINATES THE ENTIRE GULF. EXPECT MOSTLY FAIR WEATHER FOR THE NEXT 24 HOURS WITH WARMING SURFACE TEMPERATURES. THE CARIBBEAN SEA... A STATIONARY FRONT EXTENDS FROM E CUBA TO E HONDURAS ALONG 20N74W 18N82W 15N83W. WIDELY SCATTERED SHOWERS ARE WITHIN 90 NM OF THE FRONT. A 1007 MB SURFACE LOW IS OFF THE COAST OF PANAMA NEAR 12N78W. SCATTERED MODERATE CONVECTION IS FROM 9N-12N BETWEEN 80W-82W...AND FROM 12N-14N BETWEEN 76W-78W. ISOLATED MODERATE CONVECTION IS NEAR JAMAICA FROM 15N-18N BETWEEN 75W-79W. IN THE UPPER LEVELS... A RIDGE IS OVER CENTRAL AMERICA AND THE ENTIRE CARIBBEAN SEA. CONSIDERABLE UPPER LEVEL MOISTURE IS OVER THE CENTRAL CARIBBEAN BETWEEN 71W-82W. STRONG SUBSIDENCE IS OVER THE REMAINDER OF THE CARIBBEAN SEA. EXPECT THE FRONT TO DRIFT NW OVER THE W CARIBBEAN WITH LIGHT CONVECTION DURING THE NEXT 24 HOURS. A SURFACE LOW WILL ALSO DRIFT W OVER THE SW CARIBBEAN AND PRODUCE A CONSIDERABLE AMOUNT OF CONVECTION. LASTLY...MORE CONVECTION WILL ADVECT INTO THE WINDWARD ISLANDS. THE ATLANTIC OCEAN... A STATIONARY FRONT IS OVER THE W ATLANTIC FROM E OF BERMUDA TO THE WINDWARD PASSAGE ALONG 32N61W 20N74W. ISOLATED MODERATE CONVECTION IS WITHIN 90 NM E OF FRONT. A 1024 MB HIGH IS OVER THE CENTRAL ATLANTIC NEAR 32N32W. MOSTLY ELY SURFACE FLOW IS FROM 20N-30N BETWEEN 15W-60W. IN THE UPPER LEVELS... WLY ZONAL FLOW IS OVER THE W ATLANTIC N OF 20N AND W OF 60W. AN UPPER LEVEL TROUGH IS OVER THE CENTRAL ATLANTIC N OF 10N BETWEEN 50W-60W. A RIDGE IS N OF 10N BETWEEN 40W-50W. AN UPPER LEVEL LOW IS OVER THE E ATLANTIC NEAR 19N16W. CYCLONIC FLOW IS N OF 10N E OF 25W. $$ FORMOSA