WDPN33 PGTW 091500 MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI// SUBJ/PROGNOSTIC REASONING FOR TROPICAL STORM 14W (CHAN-HOM) WARNING NR 011// RMKS/ 1. FOR METEOROLOGISTS. 2. 6 HOUR SUMMARY AND ANALYSIS. SUMMARY: INITIAL POSITION: 32.3N 150.7E INITIAL INTENSITY: 35 KTS GEOGRAPHIC REFERENCE: 577 NM EAST-SOUTHEAST OF YOKOSUKA, JAPAN MOVEMENT PAST 6 HOURS: NORTHWARD AT 01 KTS SIGNIFICANT WAVE HEIGHT: 15 FEET SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION: ANIMATED PROXY VISIBLE (PROXYVIS) SATELLITE IMAGERY DEPICTS A FULLY EXPOSED LOW LEVEL CIRCULATION CENTER (LLCC), WITH NEWLY DEVELOPING, MODERATE CONVECTION IN THE NORTHEASTERN QUADRANT, ALONG A LINE OF CONVERGENCE. SINCE 0600Z THE LLCC HAS TRACKED SOUTH-SOUTHEASTWARD BEFORE TURNING SHARPLY NORTH AND RETURNING TO ITS 0600Z POSITION BY THE 1200Z HOUR, MAKING THE BEST TRACK APPEAR TO BE STATIONARY. IN THE SUBSEQUENT TWO HOURS, THE SYSTEM HAS BEGUN TO MOVE OUT TO THE NORTHWEST. A 090954Z ASCAT-B PASS SHOWED THE SYSTEM IS BARELY HOLDING ONTO TROPICAL STORM STATUS, WITH THE VAST MAJORITY OF THE VISIBLE WIND FIELD BEING 30-35 KNOTS. ANIMATED WATER VAPOR IMAGERY, ATMOSPHERIC MOTION VECTOR (AMV) ANALYSIS AND MODEL FIELD DATA SHOW AN ULL POSITIONED JUST NORTH OF THE LLCC, WITH A TROUGH EXTENDING TO THE EAST. ALSO EVIDENT IN THE WATER VAPOR IMAGERY IS A LARGE DEFORMATION ZONE EAST OF HONSHU AND A STRONG UPPER-LEVEL TROUGH CURRENTLY MOVING ACROSS HONSHU. THE PROXIMITY OF THE ULL IS INTRODUCING UPPER-LEVEL CONVERGENT FLOW ALOFT OVER TS 14W, AS WELL AS BRINGING IN DRY MID-LEVEL AIR AND MODERATE NORTHWESTERLY SHEAR, INHIBITING DEVELOPMENT. SSTS AND UPPER-LEVEL OUTFLOW CONDITIONS REMAIN GENERALLY FAVORABLE BUT ARE MORE THAN OFFSET BY THE UNFAVORABLE CONDITIONS DISCUSSED ABOVE. THE INITIAL POSITION IS ASSESSED WITH HIGH CONFIDENCE USING THE EXPOSED LLCC IN THE PROXYVIS IMAGERY. THE INITIAL INTENSITY IS ASSESSED WITH HIGH CONFIDENCE BASED ON THE SCATTEROMETER DATA PRESENTED ABOVE. INITIAL WIND RADII BASIS: SCATTEROMETER DATA CURRENT STEERING MECHANISM: WEAK STEERING PATTERN. AGENCY DVORAK AND AUTOMATED FIXES: PGTW: T2.0 - 30 KTS RJTD: T2.0 - 30 KTS RCTP: T2.0 - 30 KTS CIMSS ADT: 25 KTS AT 091200Z CIMSS AIDT: 27 KTS AT 091200Z CIMSS D-MINT: 35 KTS AT 090830Z CIMSS D-PRINT: 31 KTS AT 091130Z FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: MARGINALLY UNFAVORABLE VWS: 10-15 KTS SST: 26-27 CELSIUS OUTFLOW: WEAK EASTWARD OTHER FACTORS: PROXIMITY OF AN UPPER-LEVEL LOW (ULL) JUST NORTH OF THE SYSTEM. ANALYSIS CONFIDENCE: INITIAL POSITION: HIGH INITIAL INTENSITY: HIGH INITIAL WIND RADII: HIGH 3. FORECAST REASONING. SIGNIFICANT FORECAST CHANGES: THERE ARE NO SIGNIFICANT CHANGES TO THE FORECAST FROM THE PREVIOUS WARNING. FORECAST DISCUSSION: TS 12W HAS NOW STARTED TO MOVE OUT OF THE WEAK STEERING ENVIRONMENT, AND ACCELERATE NORTHWESTWARD ALONG THE STRENGTHENING GRADIENT ALONG THE SOUTHWESTERN FLANK OF A LOW- TO MID-LEVEL SUBTROPICAL RIDGE (STR) CENTERED SOUTHWEST OF THE ALEUTIANS. THE NORTHWESTWARD TRAJECTORY IS FORECAST TO CONTINUE THROUGH TAU 36, BEFORE THE TRACK TURNS SHARPLY WESTWARD IN RESPONSE TO THE RIDGING BUILDING IN FROM THE WEST, MERGING WITH THE RIDGE SOUTHWEST OF THE ALEUTIANS, FORMING A SINGLE RIDGE EXTENDING FROM NORTH KOREA, OVER SAKHALIN ISLAND TO SOUTHEAST OF KAMCHATKA. THE SYSTEM IS FORECAST TO MAKE LANDFALL ALONG THE EASTERN COAST OF HONSHU JUST AROUND TAU 48. AFTER MAKING LANDFALL, THE EXACT ORIENTATION OF THE RIDGE TO THE WEST, EXTENDING ROUGHLY FROM NORTH KOREA TO FAR EASTERN RUSSIA, WILL DETERMINE THE TRACK THAT TS 14W TAKES. THE ECMWF DEPICTS A MORE NORTHEASTWARD AXIS OF THE RIDGE WHICH RESULTS IN A WEST-SOUTHWEST TRAJECTORY, TAKING IT OVER TOKYO. THE BULK OF THE OTHER GLOBAL AND ENSEMBLE MODELS SHOW A FLATTER RIDGE PATTERN, WHICH RESULTS IN A MORE WESTWARD TRAJECTORY ACROSS JAPAN AND INTO THE SEA OF JAPAN. THE FORECAST MORE CLOSELY FOLLOWS THE SECOND SCENARIO, WITH THE SYSTEM EMERGING INTO THE SOJ WEST OF KANAZAWA, JAPAN BY TAU 60, BEFORE GRADUALLY TURNING SOUTHWESTWARD, MAKING A SECOND LANDFALL NEAR POHANG, SOUTH KOREA BY THE END OF THE FORECAST PERIOD. REGARDING INTENSITY, THE PROXIMITY OF THE ULL WILL CONTINUE TO INHIBIT DEVELOPMENT IN THE SHORT-TERM. AFTER TAU 18, THE TROUGH CURRENTLY MOVING OVER JAPAN WILL CUT OFF INTO AN ULL WHICH DRIVES SOUTH ALONG THE EAST COAST OF HONSHU, ULTIMATELY MOVING INTO A POSITION SOUTHWEST OF TS 14W, OPENING UP A ROBUST POLEWARD OUTFLOW CHANNEL. AT THE SAME TIME, THE SYSTEM WILL BE MOVING OVER THE WARM TONGUE ASSOCIATED WITH THE KUROSHIO CURRENT, SUPPORTING INTENSIFICATION UP TO A PEAK OF 50-55 KNOTS BY TAU 36. THE ULL MOVES SOUTHEAST OF TS 14W RAPIDLY, WHILE THE SYSTEM MOVES OVER THE OYASHIO CURRENT ALONG THE COAST OF JAPAN, RESULTING IN WEAKENING PRIOR TO LANDFALL. TERRAIN INTERACTION WILL FURTHER WEAKEN TS 14W BEFORE IT MOVES INTO THE SOJ. THE SYSTEM BEGINS SUBTROPICAL TRANSITION (STT) BY TAU 60, AND WILL COMPLETE STT BY TAU 72 AS IT ALSO WEAKENS AND DISSIPATES PRIOR TO LANDFALL IN KOREA. MODEL DISCUSSION: THE OVERALL GUIDANCE PACKAGE CONTINUES TO SHIFT SOUTHWARD WITH EACH NEW MODEL RUN, THOUGH THE ENSEMBLE MEMBER DISPERSION IS DECREASING. AS MENTIONED ABOVE, THE ECMWF REMAINS A SOUTHERN OUTLIER, TAKING THE CENTER OF THE SYSTEM OVER TOKYO. THE REMAINDER OF THE MODELS ARE CONFINED TO A 110NM WIDE ENVELOPE ROUGHLY CENTERED ON THE JTWC FORECAST TRACK. THE OVERALL TRACK ENVELOPE REMAINS THE SAME THROUGH THE REMAINDER OF THE FORECAST. THE JTWC FORECAST IS PLACED NEAR THE AI CONSENSUS MEAN, WITH MEDIUM CONFIDENCE. INTENSITY GUIDANCE IS IN GOOD AGREEMENT WITH A STEADY INTENSITY FOR 12 HOURS, FOLLOWED BY A BURST OF INTENSIFICATION THROUGH TAU 36, FOLLOWED BY RAPID WEAKENING THROUGH THE REMAINDER OF THE FORECAST. THE JTWC INTENSITY FORECAST IS SET NEAR THE CONSENSUS MEAN WITH MEDIUM CONFIDENCE. FORECAST CONFIDENCE: TRACK 00-72 HR: MEDIUM TRACK 72-120 HR: LOW INTENSITY 00-72 HR: MEDIUM INTENSITY 72-120 HR: LOW// NNNN