000 AXNT20 KNHC 161724 TWDAT TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 205 PM EDT SAT APR 15 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 1700 UTC. ...ITCZ... ITCZ AXIS IS ALONG 7N11W 2N30W INTO S AMERICA NEAR 3N52W. SCATTERED MODERATE TO STRONG CONVECTION IS LOCATED WITHIN A 60 NM RADIUS OF 2N40W AND FROM 4N TO 6N W OF 48W TO THE S AMERICA COAST. ...DISCUSSION... GULF OF MEXICO... WELL-DEFINED ELONGATED MIDDLE/UPPER LEVEL CYCLONIC CIRCULATION IS CENTERED ALONG THE SOUTHERN MEXICO COAST NEAR 16N98W. THE CIRCULATION IS DRIFTING TO THE NW AND CYCLONIC FLOW COVERS THE SW QUARTER OF THE AREA. FLOW BECOMES ANTICYCLONIC OVER THE EASTERN HALF OF THE GULF. STRONG WESTERLIES ALOFT COVER THE GULF N OF ABOUT 28N. STRONG SUBSIDENCE COVERS NOT ONLY THE ENTIRE GULF AND THE SURROUNDING REGION BUT ALSO THE E PACIFIC E OF 110W. SKIES ARE MOSTLY CLEAR OVER THE AREA EXCEPT FOR SCATTERED TO BROKEN LOW CLOUDS ALONG THE TEXAS AND SW LOUISIANA COASTLINES. CARIBBEAN SEA... THE FLOW IS PREDOMINATELY ANTICYCLONIC ALOFT OVER MOST OF THE REGION EXCEPT OVER THE NE PART. THE SUBSIDENCE NOTED ABOVE COVERS THE ENTIRE CARIBBEAN AND IS STRONGEST N OF ABOUT 18N. ONLY A FEW SCATTERED SHOWERS ARE MOVING WESTWARD ACROSS THE AREA. THE ORIGINS OF A SUBTROPICAL JET ARE OVER THE SE PART NEAR 15N68W. THE JET CONTINUES NE ACROSS THE LEEWARD ISLANDS OUT INTO THE ATLANTIC. ATLANTIC... VERY DISTINCT FEATURES ALOFT COVER THE TROPICAL AND SUBTROPICAL ATLANTIC. THE FIRST OF THESE IS A LARGE MIDDLE/UPPER LEVEL TROUGH THAT HAS ITS AXIS ALONG 62W N OF 20N WITH CYCLONIC FLOW LOCATED N OF 20N BETWEEN ABOUT 45W TO 80W. A JET EMERGES OFF OF THE UNITED STATES COAST OVER S CAROLINA...DIPS TO 28N65W...AND THEN TURNS NE THROUGH 32N56W AND OUT OF THE DISCUSSION AREA. FURTHER S IS A STRONG SUBTROPICAL JET THAT EXTENDS THROUGH THE LEEWARD ISLAND TO 23N55W TO 28N38W AND THEN DIVES SE THROUGH 18N25W. STRONGEST FLOW ALONG THE JET IS BETWEEN 45W AND 55W. OVER THE DEEP TROPICS A LARGE ANTICYCLONIC CIRCULATION AT THE MIDDLE/UPPER LEVELS IS CENTERED NEAR 12N52W. THIS FEATURE DOMINATES THE AREA S OF ABOUT 23N W OF 25W. AT THE SURFACE A 1011 MB LOW IS LOCATED NEAR 27.5N48W...MOVING NE ABOUT 15 KT. A COLD FRONT TRAILS SW FROM THE LOW TO 19N60W AND THEN BECOMES A TROUGH INTO PUERTO RICO. A PRE-FRONTAL TROUGH IS LOCATED FROM 24N50W TO 16N60W. DIVERGENCE ALOFT IS AIDING THE FORMATION OF BROKEN/OVERCAST LAYERED CLOUDS WITH SCATTERED SHOWERS AND THUNDERSTORMS N OF 27N BETWEEN 20W AND 44W. A SURFACE RIDGE OVER THE E ATLANTIC IS LOCATED THROUGH 32N27W TO 19N48W. $$ CAB