000 AXPZ20 KNHC 310905 TWDEP TROPICAL WEATHER DISCUSSION NWS NATIONAL HURRICANE CENTER MIAMI FL 1005 UTC WED MAR 30 2011 TROPICAL WEATHER DISCUSSION FOR THE EASTERN PACIFIC OCEAN FROM THE EQUATOR TO 32N...EAST OF 140W. BASED ON 0600 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 0745 UTC. ...ITCZ... THE INTERTROPICAL CONVERGENCE ZONE AXIS WAS ANALYZED FROM 08N81W TO 03N95W TO 05N117W TO 01N140W. SCATTERED MODERATE WITH ISOLATED STRONG CONVECTION WAS WITHIN 75 NM EITHER SIDE OF THE ITCZ AXIS E OF 84W TO WESTERN PANAMA. ISOLATED MODERATE CONVECTION WAS WITHIN 210 NM S OF THE ITCZ AXIS BETWEEN 114W AND 120W. ...DISCUSSION... A 1034 MB SUBTROPICAL HIGH PRES SYSTEM NEAR 36N135W EXTENDS A RIDGE INTO THE FORECAST AREA NEAR 32N133W THROUGH 19N122W TO 14N100W. FRESH NE TRADE WINDS LIE S OF THE RIDGE AXIS FROM 06N TO 28N W OF 130W ACCORDING TO THE 0614 UTC ASCAT PASS. THESE TRADES ARE FORECAST TO DISSIPATE OVER THE NEXT 24 HOUR AS THE HIGH PRES SYSTEM WEAKENS AND MIGRATES TO THE W. THE PRES GRADIENT BETWEEN THE SUBTROPICAL RIDGE AND LOWER PRES OVER NE WATERS CONTINUES TO BE STRONG ENOUGH TO SUPPORT FRESH N TO NE WINDS N OF 26N BETWEEN 122W AND 130W. THIS AREA OF WIND IS EXPECTED TO SHIFT W TODAY AS THE SUBTROPICAL HIGH SHIFTS W AND PUSHES THE TIGHTEST PRES GRADIENT W WITH IT. THE SUBTROPICAL HIGH WILL WEAKEN ENOUGH OVERNIGHT TONIGHT FOR THESE WINDS TO DIMINISH BELOW ADVISORY CRITERIA. AN UPPER TROUGH LIES FROM THE SOUTHERN TIP OF BAJA CALIFORNIA NORTHWESTWARD THROUGH THE AREA TO 33N138W THEN SOUTHWESTWARD TO AN UPPER LOW NEAR 27N141W. AN UPPER RIDGE AXIS TO ITS S LIES FROM 27N129W TO 16N125W AND WILL AMPLIFY TODAY...BREAKING THE TROUGHING OVER NORTH AMERICA AWAY FROM THE UPPER LOW JUST W OF THE FORECAST AREA. A 40-60 KT SOUTHWESTERLY UPPER JET LIES ON THE SE SIDE OF THE UPPER LOW W OF THE RIDGE AXIS. THIS JET IS TRANSPORTING SUBTROPICAL MOISTURE NORTHEASTWARD INTO THE REGION W OF THE RIDGE AND N OF 15N. THIS AREA IS MARKED BY MULTI-LEVEL CLOUDINESS...WITH A BLANKET OF STRATOCUMULUS STRETCHING OUTSIDE THIS REGION TO ENCOMPASS MUCH OF THE AREA N OF 15N W OF 115W. A DISSIPATING ANTICYCLONE ALOFT LIES OVER WESTERN NICARAGUA EXTENDS A RIDGE AXIS SOUTHWESTWARD TO 00N98W AND EXTENDS ANOTHER RIDGE AXIS THROUGH PANAMA INTO COLOMBIA. THE STRONGEST CONVECTION ALONG THE ITCZ LIES E OF 85W NEAR THE COAST OF PANAMA AND COINCIDES WITH DIFFLUENCE ASSOCIATED WITH THE RIDGE AXIS ALOFT. THIS CONVECTION IS DESCRIBED IN THE ITCZ SECTION ABOVE. FARTHER W...CONVECTION ALONG THE ITCZ IS FOCUSED JUST TO THE SW OF A SURFACE TROUGH ANALYZED ALONG 121W FROM 04N TO 10N. THIS TROUGH IS A REFLECTION OF AN UPPER TROUGH THAT STRETCHES FROM CABO CORRIENTES MEXICO TO THE EQUATOR NEAR 116W. THE CONVECTION HERE IS BEING ENHANCED BY UPPER DIFFLUENCE BETWEEN THIS TROUGH AND A RIDGE AXIS FROM 07N127W TO 00N136W. INCREASING NORTHWESTERLY WINDS ALOFT ARE CARRYING THE CONVECTIVE BLOW OFF S OF THE ITCZ. $$ SCHAUER