000 AXPZ20 KNHC 130906 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 1005 UTC SUN SEP 13 2009 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. ...TROPICAL WAVES... TROPICAL WAVE ALONG 91W/92W NORTH OF 05N MOVE WEST 15 KT. NO CONVECTION IS NOTED NEAR THE WAVE. TROPICAL WAVE ALONG 110W/111W FROM 05N TO 17N MOVE WEST 15 KT. CONVECTION IS EAST OF THE WAVE AXIS WITHIN THE ITCZ AND IS DESCRIBED IN THE ITCZ SECTION. NO ORGANIZATION OF THE CONVECTION IS NOTED. ...THE ITCZ... THE INTERTROPICAL CONVERGENCE ZONE IS ALONG THE LINE 06N77W TO 10N95W TO 10N105W TO 05N140W. SCATTERED MODERATE WITH ISOLATED STRONG CONVECTION IS WITHIN THE AREA FROM 09.5N TO 12N FROM 95W TO 101W. SCATTERED MODERATE TO STRONG CONVECTION IS WITHIN 75 NM EITHER SIDE OF A LINE FROM 14N105W TO 10N108W TO 08N114W. SCATTERED MODERATE TO STRONG CONVECTION IS WITHIN 100 NM OF THE POINT 06.5N128W. ...DISCUSSION... DEEP LAYER TROUGH IS OVER THE NORTHWEST PART OF THE AREA NORTHWEST OF A LINE FROM SOUTHERN CALIFORNIA TO 20N140W. THE AREA IS DRY AND CLOUD FREE IN THE MIDDLE AND UPPER LEVELS WITH BROKEN TO OVERCAST STRATOCUMULUS IN THE LOWER LEVELS. A WEAK COLD FRONT IS OVER THE FAR NORTHWEST PART OF THE AREA. THE TROUGH IS FORECAST TO MOVE EAST AND BE REPLACED BY NEAR ZONAL FLOW IN THE NEXT DAY OR TWO. THE COLD FRONT IS FORECAST TO WEAKEN AS IT MOVES EAST BECOMING DIFFUSE SOUTH OF 32N MONDAY. ANOTHER DEEP LAYER TROUGH EXTENDS SOUTH FROM A CYCLONIC CIRCULATION THAT IS OVER TEXAS. THE TROUGH IS EAST OF A LINE THAT EXTENDS FROM SOUTHEASTERN ARIZONA TO THE ITCZ NEAR 100W AND WEST OF A LINE THAT EXTENDS FROM SOUTHEASTERN LOUISIANA TO THE ITCZ NEAR 95W. THERE IS SOME CONVECTION IN THE ITCZ NEAR THE BASE OF THE TROUGH BUT OTHERWISE CONVECTION IS ISOLATED OVER THE WESTERN GULF OF MEXICO. SOME CONVECTION WAS OVER THE SIERRA MADRE OCCIDENTAL DURING THE DAYTIME BUT THIS CONVECTION HAS DIMINISHED TONIGHT. RECURRENCE DURING THE DAY TODAY IS LIKELY. BETWEEN THE TWO ABOVE TROUGHS A LARGE BROAD ANTICYCLONIC CIRCULATION DOMINATES THE FLOW. THE FLOW IS DIFFLUENT ALOFT ALONG THE SOUTHEASTERN PART OF THE FLOW WITH A LARGE AREA OF CONVECTION THAT IS MENTIONED IN THE ITCZ SECTION. DIFFLUENT FLOW ALOFT IS NOTED EAST OF 90W WITH MULTI LEVEL CLOUDS AND SOME EMBEDDED CONVECTION. A FLAT PRESSURE GRADIENT IS OBSERVED AT THE SURFACE WITH A WEAK RIDGE BETWEEN THE LOW THAT IS THE REMNANT OF LINDA NEAR 21N133W AND THE COLD FRONT OVER THE FAR NORTHWEST PART. $$ LL