000 AXPZ20 KNHC 182021 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 2205 UTC MON AUG 18 2008 TROPICAL WEATHER DISCUSSION FOR THE EASTERN PACIFIC OCEAN FROM THE EQUATOR TO 32N...EAST OF 140W. BASED ON 1800 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 2000 UTC. ...TROPICAL WAVES... NONE. ...ITCZ... ITCZ IS ALONG THE LINE...09N84W TO 14N100W TO 12N117W TO 12N128W TO 09N140W. SCATTERED MODERATE WITH ISOLATED STRONG CONVECTION IS WITHIN 180 NM OF THE AXIS BETWEEN 112W TO 123W AND WITHIN 210 NM S OF AXIS BETWEEN82W TO 86W. ...DISCUSSION... LOW...REMNANT OF ISELLE...LOCATED NEAR 19N117W WITH CENTRAL PRESSURE 1009 MB AND MOVING SLOWLY TO THE W. THE LOW LEVEL CIRCULATION CONTINUES TO BE WELL DEFINED WITH A QUIKSCAT PASS AT 1340 UTC SHOWING WINDS IN EXCESS OF 25 KT WITHIN 150 NM NW QUADRANT. AN AREA OF SCATTERED MODERATE AND ISOLATED STRONG CONVECTION LIES WITHIN 210 NM W SEMICIRCLE. EASTERLY SHEAR OVER THE LOW HAS FOCUSED THE CONVECTION W OF THE CENTER AND THE REMNANT OF ISELLE IS EXPECTED TO SLOWLY DIMINISH OVER THE NEXT SEVERAL DAYS DUE TO THIS SHEAR AND COOLER SEA SURFACE TEMPERATURES AS IT MOVES W. CURRENTLY...UPPER LEVEL DIFFLUENCE IS GREATEST TO THE S OF THE ISELLE REMNANT WHERE SCATTERED MODERATE AND ISOLATED STRONG CONVECTION CAN BE FOUND BETWEEN 08N AND 15N BETWEEN 111W AND 123W. WIDESPREAD CONVECTION WILL BE MORE LIKELY TO TRACK W WITH THIS REGION OF BETTER DEFINED UPPER LEVEL DIFFLUENCE AS OPPOSED TO THE SURFACE LOW CENTER OVER THE NEXT DAY OR TWO. A MID TO UPPER LEVEL TROUGH OVER NW WATERS IS EXPECTED TO LIFT NE INTO THE W COAST BUT LEAVE BEHIND AN UPPER LEVEL LOW THAT WILL RETROGRADE W OF 140W TUE INTO WED. AS THE TROUGH LIFTS OUT...THE ANTICYCLONE OVER NW MEXICO SHOULD PUSH W THROUGH THE BAJA ALONG 25N...CARRYING THE STRONG E FLOW ON ITS S EDGE FARTHER W INTO THE PACIFIC PRIMARILY BETWEEN 10N AND 20N E OF 120W. VERTICAL SHEAR IS A FACTOR DUE TO THIS RELATIVELY STRONG E FLOW ALOFT AND THIS SHOULD ACT TO INHIBIT CONVECTION OVER THIS REGION. WEAK MID LEVEL SHORTWAVE ENERGY PASSING ALONG THE E AND SE EDGE OF THE ANTICYCLONE OVER MAINLAND MEXICO SHOULD HELP TRIGGER CONVECTION...ESPECIALLY WITH AFTERNOON HEATING...WITH DEBRIS POTENTIALLY BEING PUSHED W SW UNDER THE DOMINANT NE STEERING FLOW TOWARD THE COAST. $$ SCHAUER CLARK