WDPN34 PGTW 132100 MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI// SUBJ/PROGNOSTIC REASONING FOR TROPICAL DEPRESSION 09W (WUKONG) WARNING NR 004// RMKS/ 1. FOR METEOROLOGISTS. 2. 6 HOUR SUMMARY AND ANALYSIS. SUMMARY: INITIAL POSITION: 27.8N 149.3E INITIAL INTENSITY: 30 KTS GEOGRAPHIC REFERENCE: 333 NM NORTHWEST OF MINAMI TORI SHIMA MOVEMENT PAST 6 HOURS: NORTHWARD AT 02 KTS SIGNIFICANT WAVE HEIGHT: 14 FEET SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION: ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY DEPICTS AN ELONGATED LLCC WITH FRAGMENTED CONVECTION ON THE SOUTH SIDE. AN EARLIER 131126Z ASCAT PASS CONFIRMED THE ELONGATED NATURE OF THE CIRCULATION, WITH MAX WINDS OF 30 KT ABOUT 100 NM SOUTHEAST OF THE CENTER. THE INITIAL INTENSITY IS SET AT 30 KT BASED ON THIS DATA, SUPPORTED BY AGENCY DVORAK INTENSITY ESTIMATES. WESTERLY VERTICAL SHEAR IS APPARENT, WITH THE UPPER-LEVEL CIRRUS OUTFLOW FROM TROPICAL STORM 08W STREAMING TOWARDS THE LLCC OF 09W. OVERALL, SYSTEM ORGANIZATION HAS NOT IMPROVED OVER THE PAST 12 HOURS. INITIAL WIND RADII BASIS: NOT APPLICABLE (THERE ARE NO INITIAL WIND RADII). CURRENT STEERING MECHANISM: SUBTROPICAL RIDGE TO THE NORTHEAST AGENCY DVORAK AND AUTOMATED FIXES: PGTW: T1.5 - 25 KTS RJTD: T2.0 - 30 KTS RCTP: T2.0 - 30 KTS KNES: T2.0 - 30 KTS FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: MARGINAL VWS: 15-20 KTS SST: 28-29 CELSIUS OUTFLOW: MODERATE EQUATORWARD OTHER FACTORS: DRY AIR MASS TO THE NORTHWEST ANALYSIS CONFIDENCE: INITIAL POSITION: MEDIUM INITIAL INTENSITY: MEDIUM INITIAL WIND RADII: NOT APPLICABLE 3. FORECAST REASONING. SIGNIFICANT FORECAST CHANGES: THE NEW FORECAST IS SIGNIFICANTLY FASTER THAN THE PREVIOUS FORECAST IN THE 36-72 HOUR PERIOD DUE TO MODEL GUIDANCE SHOWING A FASTER MOTION INTO THE MID-LATITUDE WESTERLIES. FORECAST DISCUSSION: TROPICAL STORM 09W (WUKONG) IS ELONGATED WITH A LARGE RADIUS OF MAXIMUM WIND, INDICATING POOR ORGANIZATION. MODERATE VERTICAL SHEAR IS FORECAST TO IMPACT WUKONG THROUGHOUT THE NEXT 24 HOURS DUE TO AN UPPER-LEVEL LOW TO THE NORTHWEST, COMBINED WITH UPPER-LEVEL OUTFLOW FROM 08W. DYNAMICAL MODELS LIKE THE GFS, HAFS-A, AND HWRF SEEM TO BE OVERZEALOUS IN THE SHORT TERM WITH WRAPPING DEEP CONVECTION AROUND THE EAST AND NORTH SIDE OF THE CIRCULATION, AS THIS HAS NOT BEEN OBSERVED YET. AS A RESULT, THE JTWC INTENSITY FORECAST IS LOWER THAN THESE MODELS, AND SHOWS A PEAK OF 35 KT DURING THE 12-36 HOUR PERIOD. AFTER 36 HOURS, THE STORM WILL MOVE OVER COOLER WATERS AND MERGE INTO THE MID-LATITUDE WESTERLIES. MOST MODELS ARE IN AGREEMENT THAT THE CIRCULATION WILL OPEN UP INTO A TROUGH AS IT TURNS EASTWARD AND GETS ABSORBED INTO THE BACKGROUND FLOW SOUTH OF THE JET STREAM. THE JTWC FORECAST THUS SHOWS DISSIPATION BY 72 HOURS, EVEN AS THE SYSTEM LIKELY RETAINS 25 KT WINDS ON ITS SOUTH SIDE. MODEL DISCUSSION: THE JTWC TRACK FORECAST IS CLOSE TO THE MULTI-MODEL CONSENSUS. THE JTWC INTENSITY FORECAST IS CLOSE TO THE STATISTICAL GUIDANCE, BUT A BIT BELOW DYNAMICAL MODELS LIKE HWRF, HAFS-A, AND GFS DUE TO THEIR POOR REPRESENTATION OF THE STORM'S CURRENT STRUCTURE. FORECAST CONFIDENCE: TRACK 0 - 72 HR: MEDIUM INTENSITY 0 - 72 HR: MEDIUM// NNNN