000 AXPZ20 KNHC 061531 TWDEP TROPICAL WEATHER DISCUSSION NWS NATIONAL HURRICANE CENTER MIAMI FL 1605 UTC FRI JUN 06 2014 TROPICAL WEATHER DISCUSSION FOR THE EASTERN PACIFIC OCEAN FROM THE EQUATOR TO 32N...EAST OF 140W. THE FOLLOWING INFORMATION IS BASED ON SATELLITE IMAGERY...WEATHER OBSERVATIONS...RADAR...AND METEOROLOGICAL ANALYSIS. BASED ON 1200 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 1300 UTC. ...INTERTROPICAL CONVERGENCE ZONE/MONSOON TROUGH... THE MONSOON TROUGH WAS ANALYZED FROM 08N78W TO 08N83W TO 10N90W TO 1007 MB LOW PRES NEAR 11N100W TO 09N114W TO 11N124W TO 1009 MB LOW PRES NEAR 11N128W. THE ITCZ AXIS WAS ANALYZED FROM 1009 MB LOW PRES NEAR 11N128W TO 05N140W. SCATTERED MODERATE TO STRONG CONVECTION WAS S OF THE AXIS TO 03N E OF 80W. SCATTERED MODERATE WITH ISOLATED STRONG CONVECTION WAS WITHIN 120 NM SW AND W QUADRANTS OF LOW PRES NEAR 11N100W. SCATTERED MODERATE CONVECTION WAS WITHIN 150 NM N OF THE AXIS BETWEEN 106W AND 114W AND WITHIN 150 NM S OF THE AXIS BETWEEN 105W AND 109W. SCATTERED MODERATE WITHIN 120 NM NW SEMICIRCLE OF LOW PRES NEAR 11N128W. ...DISCUSSION... A VAST ANTICYCLONE CENTERED NEAR 22N120W EXTENDS AN UPPER RIDGE AXIS THROUGH THE SOUTHERN TIP OF BAJA CALIFORNIA THEN SOUTHEASTWARD TO A SMALLER ANTICYCLONE NEAR 15N99W THEN EASTWARD THROUGH GUATEMALA. UPPER DIFFLUENCE ASSOCIATED WITH THIS RIDGE AXIS IS ASSISTING IN LIFTING THE MOIST AIR POOLED ALONG THE COAST OF SOUTHERN MEXICO SEEN IN PRECIPITABLE WATER IMAGERY. ISOLATED MODERATE TO STRONG CONVECTION IS NOTED WITHIN 150 NM SW OF THE COAST BETWEEN 92W AND 101W. THE ANTICYCLONE IS ALSO ENHANCING THE CONVECTION ASSOCIATED WITH A 1007 MB SURFACE LOW EMBEDDED IN THE MONSOON TROUGH NEAR 11N100W. THIS CONVECTION IS DESCRIBED IN THE SECTION ABOVE. THE MAIN ANTICYCLONE EXTENDS AN UPPER RIDGE SOUTHWESTWARD TO 14N138W...JUST E OF AN UPPER TROUGH THAT ORIGINATES FROM AN UPPER LOW NEAR 28N143W THROUGH 11N140W TO 06N120W. PRECIPITABLE WATER IMAGERY SHOWS MOISTURE POOLED NEAR A 1009 MB SURFACE LOW EMBEDDED IN THE MONSOON TROUGH/ITCZ AXIS NEAR 11N128W...UNDER THE INFLUENCE OF THE DIFFLUENCE ALOFT ASSOCIATED WITH THE UPPER RIDGE. CONVECTION NEAR THIS LOW IS DESCRIBED IN THE SECTION ABOVE. THE UPPER PATTERN IS EXPECTED TO VARY LITTLE OVER THE NEXT TWO DAYS...KEEPING THE CURRENTLY FAVORED AREAS FOR DEEP CONVECTION IN THE SAME GENERAL REGIONS. A 1031 MB SUBTROPICAL HIGH WAS ANALYZED NEAR 41N139W. THE SUBTROPICAL RIDGE EXTENDS FROM THE HIGH SOUTHEASTWARD INTO THE FORECAST AREA THROUGH 32N134W TO 25N115W. TRADE WINDS ARE PRIMARILY A MODERATE BREEZE W OF THE RIDGE AXIS...WITH A FRESH NW BREEZE CURRENTLY FOUND BETWEEN THE RIDGE AND THE BAJA CALIFORNIA COAST ACCORDING TO THE ASCAT PASS FROM AROUND 0515 UTC. THE SUBTROPICAL HIGH IS FORECAST TO STRENGTHEN AS IT DRIFTS SW OVER THE NEXT TWO DAYS. THE PRES GRADIENT BETWEEN THE RIDGE AND TROUGHING OVER THE GULF OF CALIFORNIA IS EXPECTED TO BE STRONG ENOUGH TO SUPPORT WINDS TO 25 KT N OF 28N ALONG THE BAJA CALIFORNIA COAST E OF 117W THIS AFTERNOON THROUGH EARLY SAT MORNING BEFORE THE HIGH SHIFTS FARTHER AWAY FROM THIS AREA. CROSS-EQUATORIAL SW SWELL IS MOVING INTO THE SW CORNER OF THE AREA THIS MORNING...WITH PERIODS IN THE 19-21 SECOND RANGE. THE LEADING EDGE OF THIS SWELL WILL REACH THE GALAPAGOS ISLANDS SAT MORNING AND MUCH OF THE MAINLAND COASTLINE FROM BAJA NORTE SOUTHWARD BY MIDDAY SUN. $$ SCHAUER