000 AXPZ20 KNHC 120248 TWDEP TROPICAL WEATHER DISCUSSION NWS NATIONAL HURRICANE CENTER MIAMI FL 0405 UTC FRI OCT 12 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 0000 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 0230 UTC. ...SPECIAL FEATURES... 1008 MB LOW PRES IS EMBEDDED ALONG THE MONSOON TROUGH NEAR 11.5N104W...OR 520 MILES S OF MANZANILLO MEXICO. THIS LOW HAS SCATTERED MODERATE AND ISOLATED STRONG CONVECTION WITHIN 240 NM IN THE NW QUADRANT. ENVIRONMENTAL CONDITIONS APPEAR CONDUCIVE FOR GRADUAL DEVELOPMENT OF THIS LOW DURING THE NEXT COUPLE DAYS AS IT MOVES WESTWARD AT AROUND 10 KT UNDERNEATH UPPER LEVEL RIDGING EXTENDING FROM A PARENT ANTICYCLONE OVER CENTRAL MEXICO NEAR 20N100W. IN ADDITION...ADDED VORTICITY FROM THE GULF OF TEHUANTEPEC THROUGH THE NEXT 48 HOURS ALONG WITH PERSISTENT CONVECTION MAY ALSO AID IN THE DEVELOPMENT OF THE LOW. ...INTERTROPICAL CONVERGENCE ZONE/MONSOON TROUGH... THE MONSOON TROUGH IS ALONG 09N79W TO LOW PRES NEAR 13N93.5W 1009 MB TO LOW PRES NEAR 11.5N104W 1008 MB TO 11N118W TO 10N129W. THE INTERTROPICAL CONVERGENCE ZONE AXIS EXTENDS FROM 10N129W TO 09N140W. SCATTERED MODERATE AND ISOLATED STRONG CONVECTION IS WITHIN 120 NM S OF THE MONSOON TROUGH BETWEEN 81W AND 84W...AND WITHIN 180 NM N OF THE MONSOON TROUGH BETWEEN 96W AND 100W. SCATTERED MODERATE CONVECTION IS FROM 07N TO 10N W OF 124W...AND ALSO FROM 10N TO 13N BETWEEN 132W AND 138W. ...DISCUSSION... W OF 110W...A CUTOFF UPPER LEVEL LOW NE OF POINT CONCEPTION CALIFORNIA IS MIGRATING NE-E ACROSS SOUTHERN CALIFORNIA. THIS UPPER FEATURE AND AN ATTENDANT UPPER TROUGH IS SUPPORTING A COLD FRONT EXTENDING FROM CENTRAL ARIZONA TO ACROSS THE NORTHERN GULF OF CALIFORNIA. IT IS ALSO SUPPORTING A SURFACE TROUGH TO THE W OF THE FRONT FROM E OF SAN DIEGO THROUGH 30N116W TO 26N118W. MODEL GUIDANCE INDICATES 20 TO 25 KT SW WINDS IN THE FAR NORTHERN GULF OF CALIFORNIA AHEAD OF THE APPROACHING SURFACE TROUGH TONIGHT. FOLLOWING THE TROUGH PASSAGE...A SURGE OF NORTHERLY WINDS ARE EXPECTED FIRST OVER THE SOUTHERN GULF OF CALIFORNIA FRI EVENING...EXPANDING TO THE MAJORITY OF THE GULF BY SAT EVENING AS STRONG HIGH PRES DEVELOPS OVER THE U.S. GREAT BASIN...AND LOW PRES TROUGHING SETS UP OVER NW MEXICO AND THE GULF OF CALIFORNIA REGION. MODERATE TO FRESH NORTHERLY WINDS WILL ALSO BE POSSIBLE ALONG THE W COAST OF THE BAJA CALIFORNIA PENINSULA FRI EVENING INTO THE WEEKEND. AN UPPER LEVEL SHORT WAVE TROUGH IS DIGGING E AND SE INTO THE FAR NW PORTION OF THE DISCUSSION WATERS...REACHING FROM 32N135W TO 22N140W. THIS UPPER FEATURE IS SUPPORTING A LAGGING COLD FRONT MOVING JUST N AND W OF 32N. THE SOUTHERN EXTENT OF THIS FRONT APPEARS TO BE STALLING HOWEVER...AND WILL LIKELY NOT REACH THE DISCUSSION WATERS S OF 30N THROUGH FRI. THIS SET UP WILL LEAVE A BROAD SURFACE RIDGE OVER THE AREA N OF 18N W OF THE MENTIONED SURFACE TROUGH LARGELY IN TACT THROUGH THE NEXT 48 HOURS WHICH WILL IN TURN MAINTAIN PRIMARILY MODERATE TO FRESH TRADE WIND FLOW ALONG AND S OF THE SOUTHERN EXTENT OF THE RIDGE. THE EXCEPTION WILL BE OVER THE W CENTRAL WATERS WHERE AN AREA OF FRESH TO STRONG NE TO E WINDS WERE CAPTURED BY AFTERNOON ASCAT SCATTEROMETER PASSES. THESE WINDS ARE FORECAST TO PERSIST OVER ROUGHLY THE SAME AREA THROUGH THE NEXT 48 HOURS. ALSO...THE TRADE WIND FLOW IS ENHANCING CLUSTERS OF CONVECTION ALONG THE WESTERN EXTENT OF THE MONSOON TROUGH AND THE ITCZ AS IS DESCRIBED IN THE CONVECTION SECTION. NW SWELL WITH PEAK WAVE PERIODS OF 15-17 SECONDS CONTINUES TO PROPAGATE FROM THE N CENTRAL PACIFIC INTO THE AREA...FROM 10N TO 21N W OF 123W...AND ALSO OVER THE REMAINDER OF THE AREA N OF 05N W OF 135W AS MEASURED BY EARLIER ALTIMETER PASSES. THIS SWELL WILL SINK SOUTHWARD REACHING THE EQUATOR BY 24 THROUGH 48 HOURS. E OF 110W...THE DOMINANT FEATURES ARE TWO LOW PRES AREAS ALONG THE MONSOON TROUGH...THE WESTERN LOW OF WHICH IS LISTED IN THE SPECIAL FEATURES SECTION. THE EASTERN 1009 MB LOW NEAR 13N93.5W HAS ANY ASSOCIATED CONVECTION DISPLACED WELL TO THE W DUE TO MODERATE TO STRONG UPPER LEVEL NE TO E SHEAR AND THIS LOW IS NOT EXPECTED TO DEVELOP FURTHER UNLIKE THE WESTERN LOW. $$ LEWITSKY