000 AXPZ20 KNHC 051518 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 1605 UTC THU NOV 05 2009 TROPICAL WEATHER DISCUSSION FOR THE EASTERN PACIFIC OCEAN FROM THE EQUATOR TO 32N...EAST OF 140W. BASED ON 1200 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 1500 UTC. ...ITCZ... THE INTERTROPICAL CONVERGENCE ZONE IS ALONG THE LINE...09N83W TO 09N105W TO 07N140W. SCATTERED MODERATE WITH ISOLATED STRONG CONVECTION IS WITHIN THE AREA FROM 09N TO 10N FROM 104W TO 109W. SCATTERED MODERATE WITH ISOLATED STRONG CONVECTION IS WITHIN 120 NM OF THE POINT 10N122W. SCATTERED MODERATE WITH ISOLATED STRONG CONVECTION IS WITHIN 75 NM OF THE POINT 08N126.5W. ...DISCUSSION... TWO TROUGHS DOMINATE THE MIDDLE AND UPPER LEVELS. A DEEP LAYER TROUGH IS OVER THE NORTHERN PART OF THE PACIFIC OCEAN FROM NORTHERN BAJA CALIFORNIA TO THE ITCZ NEAR 140W. THE TROUGH IS FORECAST TO MOVE EAST SLOWLY AND BECOME SLIGHTLY MORE INTENSE WITH A CYCLONIC CIRCULATION REACHING NORTHERN BAJA CALIFORNIA FRIDAY AND SLOWING FURTHER BEFORE WEAKENING OVER THE WEEKEND. AN ASSOCIATED SURFACE COLD FRONT EXTENDS FROM 32N127W TO 24N140W. SOME BROKEN MOSTLY HIGH CLOUDS ARE NORTH OF 25N FROM 123W TO 135W MAINLY ASSOCIATED WITH THE SOUTHERLY FLOW AHEAD OF THE TROUGH AXIS. THE OTHER TROUGH IS A MAINLY UPPER LEVEL TROUGH THAT EXTENDS FROM THE WESTERN GULF OF MEXICO ACROSS THE ISTHMUS OF TEHUANTEPEC TO THE ITCZ NEAR 95W. THE TROUGH AXIS IS RATHER SHARP WITH DRY AND CLOUD FREE MIDDLE AND UPPER LEVELS WITHIN 600 NM WEST OF THE TROUGH AXIS AND DIFFLUENT UPPER FLOW WITH MULTI LEVEL CLOUDS AND EMBEDDED AREAS OF CONVECTION WITHIN 300 NM EAST OF THE TROUGH AXIS. THE REMAINDER OF THE MIDDLE AND UPPER LEVELS IS COVERED BY BROAD ANTICYCLONIC FLOW. WEAK RIDGE IS NORTH OF 17N WEST OF 110W AHEAD OF THE COLD FRONT. ALSO WEAK RIDGE WEST OF THE FRONT. ELSEWHERE BROAD TROUGH IS ANALYZED AT THE SURFACE. STRONG HIGH PRES ACROSS SOUTHERN MEXICO WILL CONTINUE GALE FORCE WINDS THROUGH THE GULF OF TEHUANTEPEC THROUGH FRI AND THROUGH SATURDAY AT LESS THAN GALE FORCE. $$ LL