000 AXNT20 KNHC 150520 TWDAT TROPICAL WEATHER DISCUSSION... NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 205 AM EDT TUE APR 15 2008 TROPICAL WEATHER DISCUSSION FOR NORTH AMERICA...CENTRAL AMERICA...THE GULF OF MEXICO...THE CARIBBEAN SEA...NORTHERN 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...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 5N11W 2N20W 1N30W CROSSING THE EQUATOR NEAR 41W AND INTO NE BRAZIL NEAR 1S47W. CLUSTERS OF STRONG CONVECTION ARE WITHIN 130 NM OF THE AFRICAN COAST BETWEEN 3N AND THE AXIS. SCATTERED MODERATE TO STRONG CONVECTION IS WITHIN 210 NM N AND 140NM S OF THE AXIS BETWEEN 19W-23W. SCATTERED MODERATE TO STRONG CONVECTION IS FROM 2N-5N BETWEEN 29W-39W. ...DISCUSSION... THE GULF OF MEXICO... A STRONG COLD FRONT HAS CONTINUED TO MOVE THROUGH THE GULF THIS MORNING. AS OF 03Z...THE FRONT STRETCHED FROM THE STRAIGHTS OF FLORIDA ALONG THE NW TIP OF CUBA THROUGH THE YUCATAN CHANNEL AND OVER THE THE YUCATAN PENINSULA. THE FRONT RE-EMERGES IN THE BAY OF CAMPECHE NEAR 20N91W AND CONTINUES WNW TO NEAR 22N96W. THE FRONT IS FAIRLY DRY WITH THE ONLY SHOWERS DEVELOPING IN THE FLORIDA STRAIGHTS. COLD AIR STRATOCUMULUS CLOUDS ARE FILLING IN THE GULF BEHIND THE BOUNDARY. SHIP AND BUOY OBSERVATIONS CONTINUE TO INDICATE N TO NW WINDS 15-20 KTS BEHIND THE FRONT. EXPECT THESE WINDS TO DIMINISH LATER TODAY WITH SE RETURN FLOW INCREASING OVER THE NW WATERS AS HIGH PRESSURE OVER TEXAS SHIFTS EAST DURING THE NEXT 24 HOURS. ALOFT...NEAR ZONAL FLOW AT THE BASE OF AN UPPER TROUGH RESULTS IN STRONG SUBSIDENCE OVER THE NORTHERN GULF WATERS. THE CARIBBEAN SEA... AS OF 09Z...THE PREVIOUSLY MENTIONED COLD FRONT JUST CLIPS THE FAR NW CARIBBEAN IN THE YUCATAN CHANNEL. EXPECT THIS FRONT TO CONTINUE MOVING SE INTO THE CARIBBEAN THROUGHOUT THE DAY. NE WINDS 10-15 KT AHEAD OF THE BOUNDARY WILL SHIFT NW AND INCREASE TO 20 KT FOLLOWING THE FRONTAL PASSAGE. A STATIONARY FRONT REMAINS SITUATED OVER THE CENTRAL CARIBBEAN FROM SE CUBA NEAR 21N78W ALONG 18N82W TO HONDURAS NEAR 16N87W. LOW CLOUDS AND EMBEDDED ISOLATED SHOWERS ARE BETWEEN THE TWO BOUNDARIES. FARTHER EAST...A SFC TROUGH STRETCHING FROM THE EASTERN TIP OF THE DOMINICAN REPUBLIC TO THE COLOMBIA/VENEZUELA BORDER CONTINUES TO MOVE WESTWARD THROUGH THE CARIBBEAN. SCATTERED SHOWERS ARE WITHIN 150 NM W OF THE AXIS AND N OF 14N E OF THE AXIS. SAT IMAGERY AND SAN JUAN DOPPLER RADAR INDICATES THAT THE MOST ORGANIZED ACTIVITY IS OVER THE NRN LEEWARD ISLANDS. EXPECT THIS TROUGH TO GRADUALLY DISSIPATE AS IT INTERACTS WITH THE FRONTAL BOUNDARIES IN THE WESTERN CARIBBEAN. ALOFT...A FLATTENED UPPER RIDGE RESIDES OVER THE CARIBBEAN...KEEPING THE ATMOSPHERE STABLE. WESTERN ATLANTIC... THE WEATHER PATTERN IN THE W ATLC IS DEFINED BY THE EXISTENCE OF TWO COLD FRONTS. THE STRONGER OF THE TWO FRONTAL BOUNDARIES ENTERS THE REGION NEAR 31N70W AND CONTINUES SW OVER THE BAHAMAS NEAR 24N75W BEFORE CROSSING OVER CUBA NEAR 22N77W. MULTILAYERED CLOUDS WITH EMBEDDED SHOWERS ARE WITHIN 80 NM BEHIND THE BOUNDARY. AN AREA OF INTENSE CONVECTION WITH ISOLATED THUNDERSTORMS SURROUNDS THE BOUNDARY WITHIN 80 NM OF THE NE COAST OF CUBA. AS OF 03Z...A SECOND FRONT ENTERS THE W ATLC NEAR 31N73 AND CONTINUES OVER THE NW BAHAMAS ENTERING THE STRAIGHTS OF FLORIDA NEAR 24N81W. MUCH COOLER AND DRIER AIR IS FILTERING IN BEHIND THIS BOUNDARY. ASSOCIATED CONVECTION IS MOSTLY CONFINED TO THE AREA N OF 27N...WITH LIGHTING DATA INDICATING NUMEROUS ISOLATED THUNDERSTORMS JUST N OF THE DISCUSSION AREA. STRONG N WINDS BEHIND THE FRONT ARE EXPECTED TO REACH GALE FORCE LATER TODAY TO THE WEST OF A DEVELOPING SFC LOW PRESSURE SYSTEM NEAR 30N78W. CENTRAL AND EASTERN ATLANTIC... A BROAD DEEP-LAYERED RIDGE DOMINATES THE CENTRAL AND EAST ATLC. THE SFC HIGH PRESSURE CENTER IS LOCATED NEAR 29N42W. PATCHY CLOUDS CONTINUE TO FLOW AROUND THE RIDGE. IN THE DEEP TROPICS....AN UPPER HIGH IS SITUATED NEAR 9N34W ENHANCING CONVECTION IN THE ITCZ. WLY FLOW N OF THE UPPER RIDGE AND S OF AN UPPER TROUGH IS TRANSPORTING UPPER LEVEL MOISTURE/HIGH CLOUDS FROM S AMERICA TO AFRICA BETWEEN 11N-18N. $$ CANGIALOSI/WADDINGTON