000 AXPZ20 KNHC 072134 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 2205 UTC SAT MAR 07 2009 TROPICAL WEATHER DISCUSSION FOR THE EASTERN PACIFIC OCEAN FROM THE EQUATOR TO 32N...EAST OF 140W. BASED ON 1800 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 2300 UTC. ...ITCZ... THE INTERTROPICAL CONVERGENCE ZONE IS ALONG THE LINE...06N77W TO 04N80W TO 03N105W TO 04N140W. THERE IS NO SIGNIFICANT CONVECTION ALONG THE ITCZ. ...DISCUSSION... W OF 110W...A SHARP MID/UPPER LEVEL TROUGH EXTENDS FROM SOUTHERN CALIFORNIA TO 30N125W TO ROUGHLY 27N140W. A 100 KT JET STREAK IS EVIDENT SOUTH OF THE TROUGH IN SATELLITE DERIVED WIND INFORMATION. DIVERGENCE ALOFT ASSOCIATED WITH THE RIGHT REAR PORTION OF THE JET STREAK AND AHEAD OF ANOTHER JET ACROSS HAWAII IS SUPPORTING A WEAK SURFACE TROUGH ALONG ROUGHLY 132W FROM 15N TO 20N. THE SURFACE TROUGH WILL NOT MOVE APPRECIABLY THROUGH 48 HOURS AND WILL GRADUALLY WEAKEN. OTHERWISE A SURFACE RIDGE EXTENDS FROM 30N140W TO SOUTH OF BAJA. A QUIKSCAT PASS FROM 15Z SHOWS 20 TO 25 KT BETWEEN THE SURFACE TROUGH THE RIDGE. A JASON ALTIMETER PASS FROM 17Z SHOWED 8 TO 10 FT SEAS S OF 25N W OF 130W. THIS IS THE RESULT OF THE ENHANCED TRADES...AS WELL AS PERSISTENT LONG PERIOD NW SWELL PROPAGATING THROUGH THE AREA. SHIP OBSERVATIONS AND SCATTEROMETER DATA ALSO SHOW FRESH NORTHERLY WINDS OFF THE BAJA COAST...ON THE EASTERN EDGE OF THE SURFACE RIDGE. MEANWHILE...THE SW TO W WINDS IN THE MID AND UPPER LEVELS ARE ADVECTING A PLUME OF TROPICAL MOISTURE OVER THE SURFACE RIDGE...RESULTING IN WIDESPREAD CLOUDINESS FROM 10N TO 20N...AS WELL AS POCKETS OF LIGHT RAIN AS NOTED ON AN EARLIER SHIP REPORT. THE POSITION AND CHARACTER OF THE MID/UPPER TROUGH WILL CHANGE LITTLE THROUGH 48 HOURS. WINDS OFF BAJA WILL DIMINISH AS THE SURFACE RIDGE WEAKENS SLIGHTLY...OTHERWISE LITTLE CHANGE IS EXPECTED. E OF 110W...MAIN ISSUE REMAINS STRONG GAP FLOW THROUGH THE GULF OF PAPAGAYO AND ADJACENT WATERS TO THE WEST. SCATTEROMETER DATA FROM EARLIER IN THE DAY SHOWED 20 TO 30 KT WINDS CONTINUING...DUE TO STRONG TRADES IN THE SW CARIBBEAN. DRAINAGE FLOW ENHANCES THE OVERALL FLOW IN THE EARLY MORNING. CONVERGENCE OF THE PAPAGAYO GAP WINDS WITH SOUTHERLY FLOW S OF 04N IS SPARKING MODEST CONVECTION ALONG THE ITCZ BETWEEN 85W AND 95W. MODERATE TO FRESH NORTHERLY FLOW PERSISTS THROUGH THE ISTHMUS OF PANAMA AND INTO THE GULF OF PANAMA AS WELL. FURTHER NORTH...GAP WIND FLOW THROUGH THE GULF OF TEHUANTEPEC IS DIMINISHING BELOW 20 KT. SEAS TO 8 FT CONTINUE MAINLY S OF 10N W OF 100W...MAINLY DUE TO A MIX OF NW SWELL WITH NE SWELL FROM THE PAPAGAYO WINDS. $$ CHRISTENSEN