000 AXPZ20 KNHC 110930 TWDEP TROPICAL WEATHER DISCUSSION NWS NATIONAL HURRICANE CENTER MIAMI FL 1005 UTC SAT MAY 11 2013 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 0600 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 0900 UTC. ...INTERTROPICAL CONVERGENCE ZONE/MONSOON TROUGH... THE MONSOON TROUGH EXTENDS FROM 09N83W TO 08N91W TO 10N101W THEN TRANSITIONS TO AN ITCZ WHICH EXTENDS WEST TO 10N110W TO 06N140W. SCATTERED MODERATE TO STRONG CONVECTION IS WITHIN 60 NM OF THE ITCZ AXIS BETWEEN 109W AND 135W. ...DISCUSSION... 1028 MB HIGH PRES CENTERED NEAR 31N130W. PRES GRADIENT BETWEEN THE HIGH AND LOWER PRESSURE NEAR THE ITCZ MAINTAINING MODERATE TO FRESH TRADES N OF THE ITCZ TO 18N AND W OF 115W. THIS IS HELPING TO INCREASE CONVERGENCE INTO THE ITCZ AND PRODUCE THE ACTIVE CONVECTION ALONG THE ITCZ AS NOTED ABOVE. GENTLE TO MODERATE WINDS PREVAIL ELSEWHERE ACROSS THE FORECAST AREA. WITH WINDS GENERALLY 20 KT OR LESS...AND NO SIGNIFICANT SWELL MOVING THROUGH...SEAS REMAIN 5 TO 7 FT ACROSS MOST OF THE REGION. A WEAK LATE SEASON FRONT APPROACHING NW PART OF DISCUSSION AREA TONIGHT AND SUN WILL BECOME DIFFUSE AND WEAKEN INTO A TROUGH. THE SURFACE HIGH PRESSURE RIDGE WILL WEAKEN TONIGHT AS THIS BOUNDARY APPROACHES...THEN A STRONGER RIDGE WILL BUILD EASTWARD SUN AND MON BEHIND THE FRONTAL TROUGH. A TROUGH IN THE FAR SW CARIBBEAN WILL SLOWLY MOVE ACROSS CENTRAL AMERICA THIS WEEKEND. GAP WIND FLOW ASSOCIATED WITH THIS FEATURE WILL INTERACT WITH THE MONSOON TROUGH TO HELP INCREASE LOW LEVEL VORTICITY WITHIN THE MONSOON TROUGH. GAP WINDS THROUGH THE GULF OF TEHUANTEPEC WILL BE INDUCED MON AND TUE BY THE TROUGH AS IT SHIFTS FARTHER WEST. THIS WILL FURTHER INCREASE LOW LEVEL VORTICITY WITHIN THE MONSOON TROUGH TUE AND WED. IT IS LIKELY A LOW WILL DEVELOP ALONG THE MONSOON TROUGH AS A RESULT OF THESE INTERACTIONS...THOUGH THERE IS STILL A GREAT DEAL OF UNCERTAINTY IN THE GLOBAL MODELS REGARDING THE STRENGTH OF THIS LOW. $$ MUNDELL