000 AXNT20 KNHC 260545 TWDAT TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 205 AM EDT WED MAR 26 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 0345 UTC. ...ITCZ... ITCZ AXIS IS CENTERED ALONG 5N9W 3N20W CROSSING THE EQUATOR NEAR 32W TO 2S44W. CLUSTERS OF SCATTERED MODERATE/STRONG CONVECTION IS FROM 7N TO S OF THE EQUATOR BETWEEN 4W-37W. ...DISCUSSION... GULF OF MEXICO... BROAD UPPER TROUGH COVERS THE E HALF OF THE U.S. AND THE GULF OF MEXICO INTO THE W ATLC ALTHOUGH THE ASSOCIATED FRONT IS IN THE THE W ATLC AND CARIBBEAN. SURFACE RIDGE DOMINATES THE GULF ANCHORED OFF THE COAST OF SOUTH CAROLINA BY A 1030 MB HIGH. THIS RIDGE IS GIVING THE W GULF RETURN FLOW BANKING LOW CLOUDS ALONG THE COAST OF MEXICO AND TEXAS BUT NOT PRODUCING ANY SHOWER ACTIVITY. STRONG SUBSIDENCE AND DRY STABLE AIR DOMINATE THE GULF WITH MOSTLY CLEAR SKIES COVERING THE GULF WITH THE EXCEPTION OF BROKEN COLD AIR STRATOCUMULUS CLOUDS OVER THE CENTRAL GULF FROM 87W-92W. THE RIDGE IS EXPECTED TO REMAIN OVER THE GULF THROUGH SUN. CARIBBEAN SEA... THE UPPER TROUGH OVER THE GULF EXTENDS INTO THE NW CARIBBEAN TO THE CAYMAN ISLANDS WITH THE ASSOCIATED STATIONARY FRONT EXTENDING THROUGH THE WINDWARD PASSAGE JUST W OF JAMAICA TO FAR NE HONDURAS. THIS IS GENERATING BROKEN/OVERCAST LOW/MID CLOUDS WITH ISOLATED SHOWERS WITHIN 120 NM OF LINE FROM E TIP OF CUBA TO 12N82W ALONG THE COAST OF NICARAGUA. THE REMAINDER OF THE CARIBBEAN IS DOMINATED BY A BROAD UPPER RIDGE ANCHORED BY AN UPPER HIGH OVER THE S WINDWARD ISLANDS. MODERATE/STRONG NE TO E TRADE WINDS DOMINATE THE ENTIRE REGION. THE FRONT IS EXPECTED TO DISSIPATE LATER TODAY. ATLANTIC OCEAN... BROAD UPPER TROUGH THAT COVERS THE GULF AND INTO THE CARIBBEAN COVERS THE W ATLC WITH THE ASSOCIATED COLD FRONT ENTERING THE REGION NEAR 32N61W TO THE TURKS AND CAICOS NEAR 22N71W WHERE IT PULLS UP STATIONARY INTO THE CARIBBEAN THROUGH THE WINDWARD PASSAGE. BROKEN/OVERCAST MULTILAYERED CLOUDS WITH SCATTERED SHOWERS ARE WITHIN 120 NM OF LINE FROM 23N69W TO BEYOND 32N59W WITH BROKEN/OVERCAST LOW/MID CLOUDS AND ISOLATED SHOWERS WITHIN 150 NM W OF THE FRONT ALONG THE REMAINDER OF THE FRONT. A SURFACE RIDGE THAT COVERS THE GULF OF MEXICO INTO THE W ATLC W OF FRONT ANCHORED BY A 1030 MB OFF THE COAST OF SOUTH CAROLINA NEAR 32N79W. THE UPPER RIDGE OVER THE E CARIBBEAN EXTENDS A RIDGE AXIS THE UPPER HIGH IN THE S WINDWARD TO BEYOND 32N50W. THE REMAINDER OF THE ATLC IS DOMINATED BY AN UPPER TROUGH THAT EXTENDS FROM THE E ATLC THROUGH 32N27W SSW INTO THE TROPICS TO 13N36W WITH A HIGH AMPLITUDE RIDGE AXIS COVERING THE FAR E ATLC E OF THE CAPE VERDE ISLANDS TO INLAND OVER NW AFRICA. A BROAD SURFACE RIDGE COVERS THE REMAINDER OF THE ATLC E OF THE FRONT ANCHORED BY A PAIR OF HIGHS N OF THE REGION. $$ WALLACE