000 AXPZ20 KNHC 180905 TWDEP TROPICAL WEATHER DISCUSSION NWS NATIONAL HURRICANE CENTER MIAMI FL 1005 UTC SAT AUG 18 2012 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 0645 UTC. ...INTERTROPICAL CONVERGENCE ZONE/MONSOON TROUGH... THE MONSOON TROUGH AXIS WAS ANALYZED FROM 10N85W TO 13N99W TO 09N108W TO 13N120W TO 10N140W. SCATTERED MODERATE TO STRONG CONVECTION WAS WITHIN 150 NM N OF THE AXIS BETWEEN 88W AND 91W AND WITHIN 90 NM EITHER SIDE OF THE AXIS BETWEEN 102W AND 104W. SCATTERED MODERATE WITH ISOLATED STRONG CONVECTION WAS S OF THE AXIS TO 04N BETWEEN 93W AND 97W AND FROM 04N TO 07N BETWEEN 90W AND 93W. SCATTERED MODERATE CONVECTION WAS WITHIN 60 NM N AND 90 NM S OF THE AXIS BETWEEN 126W AND 134W. ...DISCUSSION... STRONG UPPER LEVEL WINDS CAN BE FOUND OVER MUCH OF THE FORECAST AREA THIS MORNING. AN UPPER LEVEL CYCLONE IS N OF AREA AT 41N133W AND HAS A TROUGH EXTENDING S TO A COL NEAR 23N137W. 30-40 KT WESTERLIES LIE TO THE W OF THE UPPER TROUGH AXIS WITH 40-60 KT SOUTHWESTERLIES BETWEEN THE TROUGH AND THE COAST OF CENTRAL CALIFORNIA. ANTICYCLONES ALOFT NEAR 20N149W AND OVER THE NORTHERN GULF OF CALIFORNIA NEAR 30N113W EXTEND A RIDGE BETWEEN THEM THROUGH THE AFOREMENTIONED COL. WATER VAPOR IMAGERY SHOWS STRONG SUBSIDENCE N OF 14N W OF 130W. THE ANTICYCLONE OVER THE GULF OF CALIFORNIA IS PROPELLING MID TO UPPER LEVEL MOISTURE NORTHWARD TO THE EAST OF 130W. DIFFLUENCE ASSOCIATED WITH THIS ANTICYCLONE IS ENHANCING CONVECTION OVER THE GULF OF CALIFORNIA FROM 27N TO 30N. 30-40 KT EASTERLIES LIE S OF THE EASTERN ANTICYCLONE...PRIMARILY ALONG 20N E OF 130W. FARTHER S...30-40 KT EASTERLIES DOMINATE THE REGION S OF 05N W OF 90W. THESE STRONG UPPER WINDS ARE INHIBITING THE DEVELOPMENT OF DEEP CONVECTION. THE GOES-R PROVING GROUND TROPICAL OVERSHOOTING TOPS PRODUCT AND LIGHTNING DATA SHOW MOST OF THE ACTIVE CONVECTION IN THE FORECAST AREA LIES ALONG AND S OF THE DIFFLUENT UPPER RIDGE AXIS THAT EXTENDS FROM 13N110W TO AN ANTICYCLONE NEAR 10N110W. LOW LEVEL CONFLUENCE NEAR THE MONSOON TROUGH AXIS AND SPEED CONVERGENCE S OF THE AXIS ALONG 06N BETWEEN 90W AND 96W IS POOLING THE LOW LEVEL MOISTURE. THIS MOSITURE IS BEING LIFTED BY THE DIFFLUENCE ALOFT WHICH IS ENHANCING CONVECTION. THIS CONVECTION IS DESCRIBED IN THE SECTION ABOVE. 1018 MB HIGH PRES CENTERED NEAR 31N131W IS PRESENTING AN OBSTACLE FOR THE NW MOTION OF THE REMAINS OF HECTOR. THIS LOW PRES CENTER WAS NEAR 23N117W 1009 MB AT 0600 UTC. THE HIGH IS EXPECTED TO LINGER NEAR 30N130W THE NEXT FEW DAYS. THE REMNANTS ARE EXPECTED TO DRIFT FURTHER N BEFORE DISSIPATING ON SUN. THE HIGHEST PRECIPITABLE WATER VALUES IN THE FORECAST AREA LIE BETWEEN THE HECTOR REMNANTS AND THE NORTHERN GULF OF CALIFORNIA...WITH A SURGE OF LOW LEVEL MOSITURE CURRENTLY MOVING NORTHWARD THROUGH THE GULF. SHIPS VQKR7 AND H9UY ALONG WITH THE ASCAT PASS FROM 1616 UTC AND THE OSCAT PASS FROM 1856 UTC SHOW FRESH TO STRONG NW WINDS ALONG THE COAST OF CABO CORRIENTES MEXICO DRIVEN BY THE PRES GRADIENT BETWEEN LOWER PRES OVER THE CENTRAL MEXICO AND RIDGING IN THE PACIFIC. THESE WINDS ARE FORECAST TO DIMINISH TO A FRESH BREEZE OR LESS BY AFTERNOON WHEN THE PRES GRADIENT RELAXES. $$ SCHAUER