WDPN32 PGTW 291500 MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI// SUBJ/PROGNOSTIC REASONING FOR TROPICAL STORM 11W (SHANSHAN) WARNING NR 033// RMKS/ 1. FOR METEOROLOGISTS. 2. 6 HOUR SUMMARY AND ANALYSIS. SUMMARY: INITIAL POSITION: 33.4N 131.2E INITIAL INTENSITY: 45 KTS GEOGRAPHIC REFERENCE: 70 NM SOUTHWEST OF IWAKUNI, JAPAN MOVEMENT PAST 6 HOURS: NORTHEASTWARD AT 08 KTS SIGNIFICANT WAVE HEIGHT: 0 FEET SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION: ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY AND A COMPOSITE RADAR LOOP SHOW CONTINUED RAPID EROSION AND UNRAVELING OF CONVECTIVE TOPS AND FEEDER BANDS AS THE SYSTEM TRACKS ACROSS KYUSHU. THE INITIAL POSITION IS PLACED WITH HIGH CONFIDENCE BASED ON THE DEFINED CIRCULATION ON THE RADAR LOOP AND TRIANGULATION FROM NUMEROUS SURFACE WIND OBSERVATIONS. THE INITIAL INTENSITY IS EXTRAPOLATED FROM THE SAME WIND OBSERVATIONS AND ACCOMPANYING SEA LEVEL PRESSURE REPORTS WITH MEDIUM CONFIDENCE AND SUPPORTED BY RJTD AND AUTOMATED DVORAK ESTIMATES. ANALYSIS INDICATES A HIGHLY UNFAVORABLE ENVIRONMENT DUE TO INTERACTION WITH THE RUGGED TERRAIN. INITIAL WIND RADII BASIS: SURFACE WIND OBSERVATIONS. CURRENT STEERING MECHANISM: SOUTHWEST EXTENSION OF THE SUBTROPICAL RIDGE (STR) TO THE EAST. AGENCY DVORAK AND AUTOMATED FIXES: PGTW: NO CURRENT ESTIMATE RJTD: T3.5 - 55 KTS CIMSS DPRNT: 43 KTS AT 291230Z CIMSS DMNT: 45 KTS AT 290940Z FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: HIGHLY UNFAVORABLE VWS: 10-15 KTS SST: OVER LAND OUTFLOW: STRONG POLEWARD 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 SHANSHAN WILL TRACK MORE EASTWARD ALONG THE EDGE OF A SHALLOWER SOUTHWEST EXTENSION OF THE STEERING STR TO THE EAST, AND MOSTLY OVER LAND AS IT DRAGS ACROSS THE ISLANDS OF KYUSHU INTO SHIKOKU, AND HONSHU. BY TAU 48, A SECONDARY STR TO THE WEST WILL COMPETE FOR STEERING AND PLACE THE SYSTEM IN A QUASI-STATIONARY MODE. THE HIGHLY UNFAVORABLE ENVIRONMENT WILL EVENTUALLY ERODE THE SYSTEM TO DISSIPATION BY TAU 72, POSSIBLY SOONER. HOWEVER, THERE IS ALSO A POSSIBILITY, AS INDICATED BY A FEW NUMERICAL TRACK MODELS, THAT THE SYSTEM WILL MAKE A TIGHT U-TURN BACK INTO THE PACIFIC OCEAN AND RE-INTENSIFY. MODEL DISCUSSION: THE NUMERICAL TRACK MODELS ARE IN GOOD AGREEMENT UP TO TAU 36; AFTERWARD, NVGM, GFS, AND AEMN LOOP THE VORTEX CLOCKWISE BACK OVER WATER. THE MAJORITY OF THE MODELS SLOW DOWN THE VORTEX UP TO TAU 72 BEFORE ACCELERATING IT NORTHEASTWARD THROUGH HONSHU. IN VIEW OF THESE, THERE IS ONLY MEDIUM CONFIDENCE IN THE JTWC TRACK FORECAST. GIVEN THE VARIABILITY OF A LAND TRACK AND THE POSSIBILITY OF A RETURN TO WATER, THERE IS LOW CONFIDENCE IN THE JTWC INTENSITY FORECAST. FORECAST CONFIDENCE: TRACK 0 - 72 HR: MEDIUM INTENSITY 0 - 72 HR: LOW// NNNN