WDPN33 PGTW 290900 MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI// SUBJ/PROGNOSTIC REASONING FOR TROPICAL STORM 11W (CO-MAY) WARNING NR 026// RMKS/ 1. FOR METEOROLOGISTS. 2. 6 HOUR SUMMARY AND ANALYSIS. SUMMARY: INITIAL POSITION: 28.1N 124.1E INITIAL INTENSITY: 35 KTS GEOGRAPHIC REFERENCE: 219 NM WEST-NORTHWEST OF KADENA AB MOVEMENT PAST 6 HOURS: NORTHWESTWARD AT 09 KTS SIGNIFICANT WAVE HEIGHT: 16 FEET SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION: ANIMATED MULTISPECTRAL SATELLITE IMAGERY (MSI) DEPICTS A WELL-DEFINED, YET SOMEWHAT DISORGANIZED, LOW LEVEL CIRCULATION CENTER (LLCC), WHICH IS BEGINNING TO ELONGATE AS IT TRACKS TOWARDS SHANGHAI. THE ANIMATED MSI, WHEN COMPARED TO ANIMATED WATER VAPOR IMAGERY AND A 290246Z GMI COLOR-ENHANCED 91GHZ MICROWAVE IMAGE, CLEARLY SHOW A DECOUPLING OF THE VORTEX, WITH THE MID- TO UPPER-LEVEL VORTEX POSITIONED NORTHWEST OF THE LLCC DUE TO PERSISTENT SOUTHEASTERLY SHEAR. THE MSI SHOWS THE LOWER-LEVEL CLOUD LINES TO THE SOUTH OF AN AREA OF FLARING CONVECTION, AND TRACING OF THESE CLOUD LINES, ALONG WITH RADAR DATA, PROVIDES HIGH CONFIDENCE TO THE INITIAL POSITION. THE INITIAL INTENSITY IS ASSESSED WITH MEDIUM CONFIDENCE, PLACED ROUGHLY AT THE AVERAGE OF THE AVAILABLE OBJECTIVE AND SUBJECTIVE INTENSITY ESTIMATES NOTED BELOW. EARLIER ASCAT DATA INDICATED ISOLATED POCKETS OF 35 KNOT WINDS, MOSTLY CONSTRAINED TO THE NORTHERN HEMISPHERE OF THE SYSTEM. ENVIRONMENTAL CONDITIONS ARE MARGINAL, WITH RELATIVELY LOW DEEP-LAYER SOUTHERLY SHEAR (HIGHER MID-LEVEL SHEAR), WARM SSTS EXCEEDING 28C AND WEAK POLEWARD OUTFLOW PROVIDED BY AN UPPER-LEVEL TROF OR WEAK LOW OVER EASTERN CHINA. INITIAL WIND RADII BASIS: PERSISTENCE CURRENT STEERING MECHANISM: SOUTHWESTERN PERIPHERY OF A DEEP-LAYER SUBTROPICAL RIDGE (STR) OVER CENTRAL JAPAN. AGENCY DVORAK AND AUTOMATED FIXES: PGTW: T2.0 - 30 KTS RJTD: T2.0 - 30 KTS RCTP: T2.0 - 30 KTS CIMSS SATCON: 37 KTS AT 290516Z CIMSS ADT: 35 KTS AT 290540Z CIMSS AIDT: 40 KTS AT 290540Z CIMSS D-PRINT: 31 KTS AT 290610Z FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: MARGINAL VWS: 10-15 KTS SST: 28-29 CELSIUS OUTFLOW: WEAK POLEWARD OTHER FACTORS: DRY MID-LEVEL AIR TO THE SOUTH. VORTEX DECOUPLING. ANALYSIS CONFIDENCE: INITIAL POSITION: HIGH INITIAL INTENSITY: MEDIUM INITIAL WIND RADII: MEDIUM 3. FORECAST REASONING. SIGNIFICANT FORECAST CHANGES: THERE ARE NO SIGNIFICANT CHANGES TO THE FORECAST FROM THE PREVIOUS WARNING. FORECAST DISCUSSION: TROPICAL STORM (TS) 11W IS FORECAST TO CONTINUE TRACKING NORTHWESTWARD ALONG THE SOUTHWESTERN SIDE OF THE DEEP STR SITUATED OVER THE NORTHERN COAST OF CENTRAL JAPAN THROUGH THE FORECAST PERIOD. LANDFALL IN THE VICINITY OF SHANGHAI IS ANTICIPATED SHORTLY AFTER TAU 24, AND THEREAFTER THE RAPIDLY WEAKENING REMNANTS OF TS 11W WILL CONTINUE TRACKING NORTHWESTWARD SLOWLY, ULTIMATELY COMING TO REST NEAR TAIHU LAKE BY THE END OF THE FORECAST PERIOD. IN TERMS OF INTENSITY, WHILE CONDITIONS ARE NOT FAVORABLE SIGNIFICANT INTENSIFICATION, SOME LEVEL OF MINOR INTENSIFICATION IS LIKELY AS THE SYSTEM APPROACHES THE COASTLINE, WITH A PEAK INTENSITY OF 40 KNOTS ANTICIPATED AT LANDFALL. ONCE THE SYSTEM IS ASHORE, IT WILL WEAKEN RELATIVELY QUICKLY OVER LAND, DISSIPATING AS A TROPICAL CYCLONE NEAR TAIHU LAKE BY TAU 72. THE REMNANT VORTEX ASSOCIATED WITH THE REMNANTS OF TS 11W MAY MOVE BACK OVER THE YELLOW SEA AFTER TAU 96 BUT AT THIS TIME, ARE NOT EXPECTED TO REDEVELOP. MODEL DISCUSSION: DETERMINISTIC TRACK GUIDANCE IS IN GOOD AGREEMENT ON THE OVERALL TRACK THROUGH TAU 48, WITH MINIMAL ALONG- OR CROSS-TRACK UNCERTAINTY. AFTER TAU 48, AS MODELS BEGIN TO LOSE THE VORTEX, TRACK SPREAD STARTS TO INCREASE SHARPLY, THOUGH THE BULK OF THE GUIDANCE SUPPORTS A SLOWING OF TRACK SPEED AND A SLOW TURN TO THE NORTHEAST. THE JTWC FORECAST IS POSITIONED NEAR THE MULTI-MODEL CONSENSUS MEAN THROUGH THE FORECAST PERIOD WITH HIGH CONFIDENCE. INTENSITY GUIDANCE IS ALSO IN GOOD AGREEMENT, SUPPORTING A SLIGHT INTENSIFICATION PRIOR TO LANDFALL, FOLLOWED BY RAPID WEAKENING TO DISSIPATION BY TAU 72. FORECAST CONFIDENCE: TRACK 0 - 72 HR: HIGH INTENSITY 0 - 72 HR: HIGH// NNNN