000 AXPZ20 KNHC 160913 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 1005 UTC SAT AUG 16 2008 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. ...SPECIAL FEATURE... TROPICAL DEPRESSION ISELLE 18.7N 111.6W MOVE NORTH-NORTHWEST AT 4 KNOTS AT 0900 UTC. MAXIMUM SUSTAINED WIND 30 TO 40 KT. SCATTERED MODERATE CONVECTION IS WITHIN 60 NM OF THE POINT 18.5N114.5W WHICH IS WELL WEST OF THE CENTER. ISELLE WEAKENING RAPIDLY DUE TO ITS COOLING SEA SURFACE TEMPERATURES AND INCREASED ELY WIND SHEAR ALOFT. SEE LATEST NHC FORECAST/ ADVISORY UNDER AWIPS/WMO HEADER MIATCMEP5/ WTPZ25 KNHC FOR MORE DETAILS. ...TROPICAL LOW... LOW 15N120W 1011 MB STATIONARY. CONVECTION HAS DISSIPATED NEAR THE SYSTEM AND ONLY SMALL LOW LEVEL CIRCULATION IS NOTED. NO DEVELOPMENT IS EXPECTED. ...TROPICAL WAVES... TROPICAL WAVE ALONG 112W FROM 05N TO 14N MOVE W 15 KT CONTINUES UNDER MODERATE ELY WIND SHEAR ALOFT WITH NO SIGNIFICANT ASSOCIATED CONVECTION. DEVELOPMENT IS NOT EXPECTED. TROPICAL WAVE ALONG 102W/103W FROM 05N TO 15N MOVE W 12 KT. SCATTERED MODERATE TO ISOLATED DEEP CONVECTION WITHIN 90 NM OF AXIS NORTH OF 13N. DEVELOPMENT IS NOT EXPECTED AS ELY WIND SHEAR REMAINS OVER THE SYSTEM. ...ITCZ... ITCZ AXIS IS ALONG THE LINE...07N77W TO 06N100W TO 10N115W TO 09N140W. SCATTERED MODERATE TO STRONG CONVECTION IS WITHIN THE AREA N OF 05N E OF 80W. SCATTERED MODERATE WITH ISOLATED STRONG CONVECTION IS WITHIN 90 NM OF THE POINT 03N80W. SCATTERED MODERATE WITH ISOLATED STRONG CONVECTION IS WITHIN 120 NM OF THE POINT 06N96W. ...DISCUSSION... MIDDLE AND UPPER LEVEL TROUGH IS WEST OF A LINE THROUGH 32N110W TO 30N117W TO 15N128W TO 14N140W. THE AREA IS DRY AND CLOUD FREE IN THE MIDDLE AND UPPER LEVELS WITH BROKEN TO OVERCAST STRATOCUMULUS IN THE LOWER LEVELS MOSTLY NORTH OF 17N. ELSEWHERE WEAK ANTICYCLONIC FLOW PREVAILS WITH MOIST MIDDLE AND UPPER LEVELS WITH EMBEDDED AREAS OF MULTI LEVEL CLOUDS AND AREAS OF CONVECTION. NONE OF THE CONVECTION APPEARS TO BE ORGANIZED BY LOW LEVEL CYCLONIC CIRCULATIONS. WEAK SURFACE RIDGE N OF 20N WEST OF 120W. VERY WEAK SURFACE RIDGE S OF 20N WEST OF 130W ALSO EAST OF 100W. ELSEWHERE BROAD TROUGH IS ANALYZED. $$ LL