000 AXPZ20 KNHC 270916 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 1005 UTC MON JUL 27 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... TROPICAL WAVE N OF 6N ALONG 96W MOVING W 20 KT. STRONG CONVECTION IS N OF 14N E OF THE WAVE TO 103W DUE MAINLY TO UPPER LEVEL DIFFLUENT FLOW. TROPICAL WAVE N OF 6N ALONG 105W MOVING W 15-20 KT. SCATTERED SHOWERS AND ISOLATED TSTMS ARE WITHIN 180 NM E AND 120 NM E OF THE WAVE. TROPICAL WAVE FROM 6N-16N ALONG 120W MOVING W 15-20 KT. SCATTERED MODERATE TO STRONG CONVECTION FROM 13N-15N BETWEEN 117W-120W. TROPICAL WAVE FROM 4N-12N ALONG 127W MOVING W 15-20 KT. SCATTERED MODERATE TO STRONG CONVECTION IS FROM 8N-13N BETWEEN 125W-128W. ...ITCZ... AXIS IS ALONG 8N78W 11N95W 9N100W 11N115W 6N140W. SCATTERED STRONG CONVECTION WITHIN 110 NM S OF AXIS E OF 80W. SCATTERED MODERATE TO STRONG CONVECTION WITHIN 120 NM S OF AXIS FROM 109W-118W. SCATTERED MODERATE ISOLATED STRONG CONVECTION WITHIN 180 NM N AND 60 NM S OF AXIS FROM 125W-135W. ...DISCUSSION... AN UPPER LEVEL TROUGH EXTENDS FROM CYCLONIC CIRCULATION N OF THE DISCUSSION AREA NEAR 35N138W WITH TROUGH FROM THE CIRCULATION TO 32N138W TO 10N130W. HIGH LEVEL MOISTURE IS ROTATING AROUND THE CYCLONIC CIRCULATION AND TROUGH. OTHERWISE MODERATE TO STRONG SUBSIDENCE WITH DRY STABLE AIR AT THE MIDDLE AND UPPER LEVELS OF THE ATMOSPHERE IS N OF THE ITCZ TO 25N BETWEEN 122W-133W. A LARGE UPPER ANTICYCLONIC CIRCULATION IS CENTERED OVER NW MEXICO NEAR 19N112W WITH A RIDGE EXTENDING S ACROSS BAJA CALIFORNIA THEN INTO THE PACIFIC TO 15N115W. SLY FLOW AROUND THE WESTERN PERIPHERY OF THE ANTICYCLONIC CIRCULATION IS ADVECTING HIGH LEVEL MOISTURE FROM ITCZ CONVECTION TO SOUTHERN CALIFORNIA. A SHARP UPPER LEVEL TROUGH WITH AXIS THAT EXTENDS FROM THE N CENTRAL GULF OF MEXICO ACROSS CENTRAL MEXICO TO A CYCLONIC CIRCULATION OFF THE W CENTRAL COAST OF MEXICO NEAR 18N105W. AN UPPER LEVEL ANTICYCLONIC CIRCULATION HAS MOVED OVER GULF OF TEHUANTEPEC NEAR 15N95W. DIFFLUENT FLOW ALOFT BETWEEN THE UPPER TROUGH AND THE ANTICYCLONIC CIRCULATION IS ENHANCING STRONG CONVECTIVE ACTIVITY NW OF THE GULF OF TEHUANTEPEC. SURFACE RIDGE WITH AXIS FROM 32N137W TO 17N105W. BROKEN/OVERCAST STRATOCUMULUS CLOUDS COVER THE AREA N OF 20N W OF 120W. LARGE SOUTHERLY SWELLS THAT HAVE BEEN CROSSING THE EQUATOR FROM THE SOUTHERN HEMISPHERE THE PAST SEVERAL DAYS OVER THE SE PORTION OF THE DISCUSSION AREA ARE STARTING TO SUBSIDE. $$ DGS