000 AXPZ20 KNHC 121529 TWDEP TROPICAL WEATHER DISCUSSION NWS NATIONAL HURRICANE CENTER MIAMI FL 1605 UTC THU MAY 12 2011 TROPICAL WEATHER DISCUSSION FOR THE EASTERN PACIFIC OCEAN FROM THE EQUATOR TO 32N...EAST OF 140W. BASED ON 1200 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 1500 UTC. ...ITCZ... THE INTERTROPICAL CONVERGENCE ZONE AXIS IS ALONG 09N104W TO 06N125W TO 04N140W. NO SIGNIFICANT CONVECTION. SCATTERED MODERATE TO ISOLATED STRONG CONVECTION IS NOTED N OF 03N E OF 94W IN A WEAK MONSOONAL FLOW. ...DISCUSSION... A TROUGH/RIDGE PATTERN DOMINATES THE FORECAST REGION. A CUT-OFF LOW IS CENTERED NEAR 26N129W WITH A TROUGH EXTENDING SW TO 23N140W. AN 70-90 KT JETSTREAM IS SE OF THE CYCLONIC CIRCULATION FROM 20N130W TO 25N120W THEN ACROSS CENTRAL BAJA CALIFORNIA AND THROUGH NORTHERN MEXICO. A BROAD ANTICYCLONIC CIRCULATION IS NEAR 13N104W AND DOMINATES THE AREA S OF 20N E OF 115W INCLUDING SOUTH-CENTRAL MEXICO AND NORTHERN CENTRAL AMERICA. A DIFFLUENT PATTERN ALOFT BETWEEN THIS ANTICYCLONE AND THE TAIL END OF A TROUGH EXTENDING ACROSS THE CENTRAL CARIBBEAN INTO THE EPAC THROUGH PANAMA IS HELPING TO MAINTAIN THE CONVECTION IS OF 94W. HIGH PRES NW OF AREA EXTENDS A RIDGE OVER THE FORECAST WATERS COVERING THE REGION N OF 15N W OF 113W. THE RIDGE COMBINED WITH LOW PRES OVER MEXICO IS PRODUCING NW WINDS OF 20 KT ALONG THE COAST OF BAJA CALIFORNIA. AN EARLIER ASCAT PASS AND A FEW SHIP OBSERVATIONS VERIFIED THE PRESENCE OF THESE WINDS WHICH ARE FORECAST TO BE BELOW 20 KT IN ABOUT 6 HOURS. AN AREA OF FRESH TRADE WINDS IS ALSO NOTED ON THE SOUTHERN PERIPHERY OF THE RIDGE PARTICULARLY FROM 07N TO 17N W OF 128W. THE RIDGE IS EXPECTED TO WEAKEN AS A COLD FRONT MOVES INTO THE NW CORNER OF THE AREA THIS SAT. AS A RESULT...THE AREAL EXTENT OF THE TRADES WILL DECREASE. A WEAK 1009 MB LOW PRES IS WITHIN THE ITCZ NEAR 9N104W. FIRST LIGHT VISIBLE IMAGERY SHOWS A WELL DEFINED SWIRL OF LOW CLOUDS ASSOCIATED WITH THE LOW CENTER WHILE MOST OF THE CONVECTIVE ACTIVITY IS TO THE W OF THE CENTER COVERING FROM 9N-12N BETWEEN 104W-107W. $$ GR