000 AXPZ20 KNHC 300238 TWDEP TROPICAL WEATHER DISCUSSION NWS NATIONAL HURRICANE CENTER MIAMI FL 0405 UTC FRI AUG 30 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 0000 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 0230 UTC. ..INTERTROPICAL CONVERGENCE ZONE/MONSOON TROUGH... THE MONSOON TROUGH EXTENDS FROM 09N84W TO 08N95W TO 11N107W. IT RESUMES AT 18N114W TO 1007 MB LOW PRES NEAR 16N115W TO 11N122W TO 1008 MB LOW PRES NEAR 12N131W TO BEYOND 10N140W. SCATTERED MODERATE ISOLATED STRONG CONVECTION WAS NOTED WITHIN 120 NM S OF TROUGH BETWEEN 84W AND 94W. SCATTERED MODERATE CONVECTION WAS NOTED WITHIN 120 NM S AND 150 NM N OF TROUGH BETWEEN 103W AND 108W. SCATTERED MODERATE ISOLATED STRONG CONVECTION WAS NOTED WITHIN 180 NM S SEMICIRCLE OF LOW PRES NEAR 16N115W. SCATTERED MODERATE ISOLATED STRONG CONVECTION WAS NOTED WITHIN 180 NM SW SEMICIRCLE OF LOW NEAR 12N131W. ...DISCUSSION... RECENTLY DOWNGRADED TROPICAL DEPRESSION JULIETTE WAS CENTERED NEAR 26.7N 114.8W AT 30/0300 UTC MOVING NW AT 12 KT. MAXIMUM SUSTAINED WIND SPEED IS 25 KT WITH GUSTS TO 35 KT. ESTIMATED MINIMUM PRESSURE IS 1008 MB. THE SYSTEM WILL CONTINUE TO WEAKEN AS IT MOVES OVER COOLER SEA SURFACE TEMPERATURES AND INTO A MORE STABLE ATMOSPHERIC ENVIRONMENT. SATELLITE IMAGERY SHOWS THAT THERE IS NO SIGNIFICANT CONVECTION WITH THE SYSTEM. THE SYSTEM IS FORECAST TO WEAKEN TO A REMNANT LOW DURING THE OVERNIGHT HOURS. A WEAK 1018 MB HIGH IS ANALYZED NEAR 27N134W. TWO LOW PRESSURE CENTERS ARE EMBEDDED WITHIN THE BROAD MONSOON TROUGH CIRCULATION...ONE NEAR 16N115W AND THE OTHER NEAR 12N131W. SATELLITE IMAGERY DEPICTS THE MONSOON TROUGH BREAKDOWN PROCESS PROGRESSING WITH THE DEEPEST CONVECTION FAVORING THE CIRCULATION AROUND THE LOW PRESSURE CENTERS AS NOTED IN THE ITCZ/MONSOON TROUGH SECTION ABOVE. THE BREAKDOWN OF THE MONSOON TROUGH WILL CONTINUE OVER THE NEXT COUPLE OF DAYS. THE EASTERN LOW IS THE LARGER OF THE TWO...BUT THE WESTERN LOW IS THE STRONGER FEATURE. THE EARLIER ASCAT PASS DEPICTED 30 KT WINDS IN THE SOUTH SEMICIRCLE AND 25 KT IN THE N SEMICIRCLE OF THE WESTERNMOST LOW. THE BREAKDOWN OF THE MONSOON TROUGH DOES NOT ALWAYS RESULT IN TROPICAL CYCLOGENESIS...AND PER THE LATEST NHC TROPICAL WEATHER OUTLOOK BOTH OF THESE LOWS HAVE A LOW CHANCE OF DEVELOPING INTO A TROPICAL CYCLONE OVER THE NEXT 48 HOURS. $$ AL