000 AXPZ20 KNHC 280926 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 1005 UTC THU MAY 28 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 0900 UTC. ...TROPICAL WAVES... A TROPICAL WAVE IS ALONG 85W/86W N OF 02N EXTENDING NORTH TO WESTERN NICARAGUA. THE WAVE IS MOVING WEST AT 15-20 KT. ASSOCIATED CONVECTION IS NORTH OF 05N AND THE CONVECTION APPEARS TO BE MOVING WEST OF THE WAVE AND NOT TENDING TOWARD AN ORGANIZED PATTERN NEAR THE WAVE. ...ITCZ... THE INTERTROPICAL CONVERGENCE ZONE IS ALONG THE LINE...07N77W TO 07N110W TO 08N120W TO 03N135W TO 03N140W. SCATTERED MODERATE TO STRONG CONVECTION IS WITHIN 120 NM OF THE POINT 08N86.5W. SCATTERED MODERATE WITH ISOLATED STRONG CONVECTION IS WITHIN 150 NM OF THE POINT 08N98.5W. SCATTERED MODERATE TO STRONG CONVECTION IS WITHIN THE AREA FROM 05N TO 080N FROM 109W TO 116W. ...DISCUSSION... UPPER LEVELS WEAK TO MODERATE WESTERLIES ARE NORTH OF 18N WITH BROAD FLAT ANTICYCLONE SOUTH OF 18N. TWO SHORTWAVES ARE WITHIN THE WESTERLIES ONE IS NORTH AND EAST OF A LINE FROM THE BIG BEND REGION OF TEXAS ACROSS CENTRAL MEXICO TO 20N117W TO 32N117W. THIS AREA IS DRY AND CLOUD FREE IN THE MIDDLE AND UPPER LEVELS EXCEPT FOR SOME CONVECTION AT THE EAST END OF THE WAVE THAT IS OVER TEXAS. ANOTHER SHORTWAVE IS OVER THE NORTH CENTRAL PART OF THE AREA NORTH OF 20N FROM 120W TO 133W. A CYCLONIC CIRCULATION IS WITHIN THIS TROUGH AND IS CENTERED NEAR 31.5N126W AND IS MOVING EAST NORTHEAST AT ABOUT 20 KNOTS. THIS FEATURE SHOULD CONTINUE THIS MOTION AND REACH SOUTHERN CALIFORNIA FRIDAY. AT THIS TIME THERE IS LITTLE WEATHER ASSOCIATED WITH THE FEATURE. THE OVERALL PATTERN WILL NOT CHANGE MUCH IN THE NEXT SEVERAL DAYS. DIFFLUENT FLOW ALOFT EAST OF A LINE FROM 15N105W TO THE ITCZ NEAR 120W IS ENHANCING THE AREAS OF CONVECTION MENTIONED IN THE ITCZ SECTION. SURFACE WEAK SURFACE RIDGE IS NORTH OF THE ITCZ WEST OF 110W. EXCEPT FOR THE TROPICAL WAVE THE REMAINDER OF THE AREA IS ANALYZED AS A WEAK TROUGH. $$ LL