000 AXPZ20 KNHC 012158 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 2205 UTC MON JUN 01 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 2100 UTC. ...ITCZ... AXIS FROM 09N85W TO 11N95W TO 05N110W TO 09N135W TO 06N140W. SCATTERED CONVECTION FROM 08N TO 11N BETWEEN 103W AND 105W. ...DISCUSSION... N OF 20N...1019 MB SURFACE PRES IS REMAINING STATIONARY NEAR 28N127W...AHEAD OF A COLD FRONT THAT EXTENDS FROM 30N129W TO 27N130W TO 25N136W...THEN STATIONARY TO 23N140W. THE FRONT IS RELATED TO A DEEP LAYER CIRCULATION NEAR 38N136W. A WEAK SECONDARY SURGE IS EVIDENT ON SATELLITE IMAGERY FROM 30N132W TO 28N140W...ALTHOUGH AN EARLIER QUIKSCAT PASS SHOWED ONLY 15 KT FLOW TO THE NORTH OF THE LINE. THE FRONT WILL STALL AND DISSIPATE OVER THE NEXT COUPLE OF DAYS AS THE THE ASSOCIATED CUTOFF LOW NORTH OF THE AREA REMAINS QUASI-STATIONARY. THE MAIN IMPACT AT THE SURFACE WILL BE A SMALL SWATH OF NORTHERLY WINDS OFF THE CENTRAL BAJA COAST THAT WILL REACH 20 KT INTO LATE THIS WEEK. S OF 20N...A SURFACE TROUGH ALONG ROUGHLY 135W FROM 05N TO 11N...ON THE SE SIDE OF A CUTOFF UPPER LOW CENTERED NEAR 16N140W. DIVERGENT FLOW ALOFT ON THE SE SIDE OF TH E UPPER LOW IS ENHANCING AN ACTIVE AREA OF CONVECTION ALONG THE FRONT FROM 11N TO 13N BETWEEN 130W AND 135W. THIS CONVECTION IS BEING FURTHER ENHANCED BY LOW LEVEL CONVERGENCE DELIVERED BY A BAND OF 20 KT TRADE WINDS SHOWING UP ON A 1430Z QUIKSCAT PASS...FROM 11N TO 16N W OF 127W. THESE TRADE WINDS ARE ON THE SOUTH SIDE OF THE 1019 MB HIGH PRES NEAR 28N127W. A 1010 MB LOW PRES IS CENTERED NEAR 07N99W...ALONG A SURFACE TROUGH FROM 11N96W TO 05N101W. ONLY MODEST CONVECTION IS EVIDENT NEAR THIS LOW PRES...GENERALLY DUE TO THE LIMITED DEEP LAYER MOISTURE AND STRONG WESTERLY SHEAR. FURTHER EAST...A 16Z ASCAT PASS SHOWED ONLY 15 KT GAP WIND FLOW THROUGH THE GULF OF PAPAGAYO. THIS IS EXPECTED TO INCREASE STARTING TONIGHT...DUE TO A SURGE OF FRESH TO STRONG TRADE WIND FLOW THROUGH THE CARIBBEAN BASIN. $$ CHRISTENSEN