WDPN31 PGTW 231500 MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI// SUBJ/PROGNOSTIC REASONING FOR TROPICAL DEPRESSION 17W (TALAS) WARNING NR 008// RMKS/ 1. FOR METEOROLOGISTS. 2. 6 HOUR SUMMARY AND ANALYSIS. SUMMARY: INITIAL POSITION: 33.0N 136.0E INITIAL INTENSITY: 30 KTS GEOGRAPHIC REFERENCE: 199 NM SOUTHWEST OF CAMP FUJI MOVEMENT PAST 6 HOURS: NORTH-NORTHEASTWARD AT 12 KTS SIGNIFICANT WAVE HEIGHT: 15 FEET SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION: ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY DEPICTS A FULLY EXPOSED LOW-LEVEL CIRCULATION CENTER (LLCC) SHEARED FROM THE MAIN BODY OF CONVECTION. ALL OF THE CONVECTIVE STRUCTURE IS NORTHEAST OF THE LLCC OVER MAINLAND HONSHU, LEAVING THE LLCC A MERE 35NM SOUTHEAST OF KUSHIMOTO, JAPAN. AN OLDER 230841Z SSMIS 91GHZ MICROWAVE IMAGE INDICATES THE CONVECTION OVER THE KANTO PLAIN REGION. THE INITIAL POSITION IS PLACED WITH HIGH CONFIDENCE BASED ON EIR LOOP AND EXTRAPOLATION FROM THE PREVIOUSLY MENTIONED MICROWAVE IMAGE. THE INITIAL INTENSITY OF 30 KTS IS ASSESSED WITH MEDIUM CONFIDENCE AND HELD WITH A MAJORITY OF MULTIPLE AGENCY DVORAK INTENSITY ESTIMATES. THE STRONG POLEWARD OUTFLOW REMAINS THE ONLY ENVIRONMENTAL CONDITION FAVORABLE, WITH ALL OTHER CONDITIONS HINDERING THE SYSTEM, INCLUDING STRONG VWS AND COOLER SSTS. INITIAL WIND RADII BASIS: PERSISTENCE CURRENT STEERING MECHANISM: SUBTROPICAL RIDGE (STR) TO THE EAST-SOUTHEAST AGENCY DVORAK AND AUTOMATED FIXES: PGTW: T2.0 - 30 KTS RJTD: T2.0 - 30 KTS CIMSS SATCON: 44 KTS AT 230842Z CIMSS ADT: 30 KTS AT 231150Z FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: UNFAVORABLE VWS: 20-25 KTS SST: 26-27 CELSIUS OUTFLOW: STRONG POLEWARD ANALYSIS CONFIDENCE: INITIAL POSITION: HIGH INITIAL INTENSITY: MEDIUM INITIAL WIND RADII: LOW 3. FORECAST REASONING. SIGNIFICANT FORECAST CHANGES: THERE ARE NO SIGNIFICANT CHANGES TO THE FORECAST FROM THE PREVIOUS WARNING. FORECAST DISCUSSION: TD 17W IS SHRINKING IN INTENSITY BASED ON THE OVERALL UNFAVORABLE ENVIRONMENT, WITH VERTICAL WIND SHEAR (VWS) INHIBITING ANY DEVELOPMENT AND THE COOLER SSTS. THE SYSTEM IS FORECAST TO CONTINUE ON A NORTHEAST TRACK UNTIL REACHING LANDFALL NEAR EITHER TOYOHASHI OR HAMAMATSU, JAPAN, BY TAU 12. THE SYSTEM WILL BEGIN DISSIPATING ONCE LAND INTERACTION OCCURS AND THE APPROACHING UPPER-LEVEL TROUGH NORTHWEST OF THE SYSTEM. THIS INTERACTION BETWEEN THE SYSTEM AND THE UPPER-LEVEL FEATURE WILL INCREASE VERTICAL WIND SHEAR (VWS), DISRUPTING THE SYSTEMS TROPICAL CONVECTIVE STRUCTURE. BY TAU 36, 17W WILL COMPLETELY DISSIPATE OVER WATER, IF NOT SLIGHTLY SOONER. MODEL DISCUSSION: NUMERICAL MODEL GUIDANCE REMAINS IN TIGHT AGREEMENT EXCLUDING NVGM AND JGSM, WHICH REMAIN THE SOLE RIGHT OUTLIERS OF THE MODEL ENVELOPE. THE CROSS-TRACK SPREAD IS ONLY 35NM UP TO TAU 24 EXCLUDING NVGM AND JGSM. DUE TO THE WEAK LLC, THE MODELS ARE STRUGGLING TO RESOLVE THE EXIT OF THE WEAK CIRCULATION BACK OUT OVER WATER. THUS, THE JTWC OFFICIAL TRACK FORECAST IS PLACED WITH MEDIUM CONFIDENCE. THE JTWC INITIAL INTENSITY IS CLOSE TO THE MULTI-MODEL CONSENSUS WITH MEDIUM CONFIDENCE THROUGHOUT THE FORECAST PERIOD. FORECAST CONFIDENCE: TRACK 0 - 72 HR: MEDIUM INTENSITY 0 - 72 HR: LOW// NNNN