000 AXPZ20 KNHC 110907 TWDEP TROPICAL WEATHER DISCUSSION NWS NATIONAL HURRICANE CENTER MIAMI FL 1005 UTC WED MAY 11 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 0845 UTC. ...ITCZ... AXIS EXTENDS FROM EMBEDDED 1008 MB LOW PRES NEAR 08N86W TO ANOTHER 1008 MB LOW PRES NEAR 09N103W TO 09N110W TO 05N125W TO 07N135W TO 05N0140W. SCATTERED MODERATE TO ISOLATED STRONG CONVECTION S OF AXIS FROM 02N TO 07N BETWEEN 85W AND 95W. SCATTERED MODERATE CONVECTION WITH 120 NM S OF AXIS BETWEEN 95W AND 105W. ...DISCUSSION... W OF 110W...AN UPPER RIDGE N OF HAWAII IS BREAKING DOWN AHEAD OF AN ADVANCING UPPER TROUGH PUSHING EASTWARD INTO THE NE PACIFIC. THIS IN TURN HAS WEAKENED A SURFACE HIGH PRES AREA NE OF HAWAII AS A COLD FRONT ASSOCIATED WITH THE UPPER TROUGH MOVES SE FROM THE N CENTRAL PACIFIC. AS A RESULT TRADE WIND FLOW BETWEEN THE ITCZ AND 20N W OF 120W CONTINUES TO DIMINISH. ASCAT PASSES FROM LATE YESTERDAY SHOWED BASICALLY 10 TO 15 KT TRADE WINDS. A PAIR OF ALTIMETER PASSES FROM YESTERDAY CONFIRMED WAVEWATCH INITIALIZATIONS SHOWING GENERALLY 5 TO 6 FT SEAS OVER THE DISCUSSION AREA W OF 110W. 20 KT NW FLOW ALONG THE COAST OF BAJA CALIFORNIA IS ALSO STARTING TO DIMINISH AS THE HIGH PRES TO THE WEST WEAKENS. LOOKING AHEAD...WHILE THE FRONT WILL STALL AND DISSIPATE N OF 30N...NEW HIGH PRES BUILDING EASTWARD BEHIND THE FRONT WILL A SMALL AREA OF 20 KT NE TRADES WILL FORM NEAR THE ITCZ W OF 130W BY LATE FRI...AHEAD OF A PAIR OF WEAK SURFACE TROUGHS MIGRATING WESTWARD ALONG THE ITCZ. SUBSIDENT DRY AIR IN THE MID AND UPPER LEVELS ALONG WITH LITTLE MAJOR TRADE WIND CONVERGENCE IN THE LOW LEVELS WILL LIMIT CONVECTION ALONG THE ITCZ. E OF 110W...BANDS OF CONVECTION CONTINUE TO PULSE AROUND A STATIONARY 1008 MB LOW PRES AREA CENTERED ALONG THE ITCZ NEAR 09N103W. CONVECTION IS AIDED BY UPPER LEVEL OUTFLOW FROM A DEVELOPING UPPER ANTICYCLONE DIRECTLY OVER THE LOW LEVEL CIRCULATION. FURTHER EAST...ANOTHER 1009 MB LOW PRES IS CENTERED NEAR 08N85W. CONVERGENCE OF MODERATE CROSS-EQUATORIAL SW FLOW INTO THESE LOW PRES AREAS IS RESULTING IN CLUSTERS OF CONVECTION FLARING TO THE S OF THE ITCZ BETWEEN 85W AND 95W. BOTH OF THESE SURFACE FEATURES WEAKEN THROUGH THE REMAINDER OF THE WEEK AS CONDITIONS ALOFT BECOME LESS FAVORABLE FOR CONVECTIVE GROWTH. $$ CHRISTENSEN