000 AXPZ20 KNHC 062125 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 2205 UTC TUE JUN 06 2006 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 1800 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 2100 UTC. ...TROPICAL WAVES... TROPICAL WAVE ALONG 83W N OF 2N MOVE W 10 KT. THE WAVE IS IN AN AREA OF EXTENSIVE CONVECTION WITHIN 240 NM OF THE CENTRAL AMERICAN COAST. HOWEVER THE AREA NEAR THE WAVE DOES NOT SHOW ANY UNUSUAL CONCENTRATION OF CONVECTION AND THE CONVECTION NEAR THE WAVE IS NOT ORGANIZED. UPPER LEVEL FLOW IS STRONG NORTHEAST AND IS NOT FAVORABLE FOR DEVELOPMENT BECAUSE OF THE STRONG NE SHEAR ALOFT. TROPICAL WAVE ALONG 102W FROM 6N TO 14N MOVING W 10 KT. MINOR ISOLATED CONVECTION WITHIN 120 NM W OF WAVE WITH NO SIGNS OF ORGANIZATION AND UPPER LEVEL NORTHEASTERLY SHEAR IS UNFAVORABLE FOR DEVELOPMENT. ..ITCZ... INTERTROPICAL CONVERGENCE ZONE ALONG...5N77W 8N105W 6N140W. SCATTERED MODERATE WITH ISOLATED STRONG CONVECTION IS WITHIN 240 NM OF THE CENTRAL AMERICAN COAST FROM 5N TO 16N. SCATTERED MODERATE WITH ISOLATED STRONG CONVECTION IS WITHIN THE AREA FROM 8N TO 11.3N FROM 105W TO 113W. ...DISCUSSION... UPPER LEVELS... BROAD CYCLONIC CIRCULATION REMAINS OVER THE AREA NORTH OF 20N EAST OF 125W. MOST OF THE CLOUDINESS ASSOCIATED WITH THIS SYSTEM HAS MOVED NORTH OVER SOUTHERN CALIFORNIA. THE CYCLONIC CIRCULATION CENTER IS NOT NEAR THE CLOUDINESS AND IS CENTERED NEAR 27.6N116W. THE SYSTEM IS EXPECTED TO CHANGE LITTLE IN THE NEXT 24 HOURS THEN WEAKEN AND MOVE NORTHWARD. A NARROW RIDGE IS BETWEEN THE ABOVE CIRCULATION AND A TROUGH NORTH OF 22N WEST OF 130W. THIS AREA IS MOIST IN THE UPPER LEVELS BUT CLOUD FREE IN THE MIDDLE AND UPPER LEVELS. THE SURFACE IS COVERED BY OVERCAST STRATOCUMULUS CLOUDS. SOUTH OF THE ABOVE SYSTEMS THE HEIGHT FIELD IS RATHER FLAT. THE AREA WEST OF 108W BETWEEN THE TROUGH TO THE NORTH AND THE ITCZ TO THE SOUTH IS OBSERVED TO BE DRY IN THE MIDDLE AND UPPER LEVELS. EAST OF 108W THERE IS EXTENSIVE CONVECTION WITHIN 240 NM OF THE CENTRAL AMERICAN COAST WITH STRONG UPPER LEVEL NORTHEASTERLY FLOW. THE AREA IS DIFLUENT ALOFT WITH MULTI LEVEL CLOUDS OVER THE AREA EAST OF 108W. SURFACE... WEAK RIDGE IS NORTH OF 17N WEST OF 115W. REMAINDER OF AREA IS A WEAK BROAD TROUGH. $$ LL