WDPN31 PGTW 012100 MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI// SUBJ/PROGNOSTIC REASONING FOR TYPHOON 14W (KOINU) WARNING NR 010// RMKS/ 1. FOR METEOROLOGISTS. 2. 6 HOUR SUMMARY AND ANALYSIS. SUMMARY: INITIAL POSITION: 18.8N 128.0E INITIAL INTENSITY: 80 KTS GEOGRAPHIC REFERENCE: 462 NM SOUTH OF KADENA AB MOVEMENT PAST 6 HOURS: NORTHWESTWARD AT 06 KTS SIGNIFICANT WAVE HEIGHT: 31 FEET SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION: ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY SHOWS TYPHOON (TY) 14W (KOINU) CONTINUING TO SLOWLY CONSOLIDATE, THOUGH THE EYE THAT WAS EVIDENT EARLIER, HAD IN THE SIX HOURS UP TO 1800Z, FILLED IN. AT THE 011800Z HOUR, EIR DEPICTED AN IRREGULAR CENTRAL DENSE OVERCAST (CDO) WITH DEEP FLARING CONVECTION PARTICULARLY NOTABLE IN THE SOUTHERN HEMISPHERE. SUBSEQUENT EIR INDICATES THE CONVECTIVE HOT TOWERS ARE STARTING TO WRAP UPSHEAR ON THE EAST SIDE OF THE LOW LEVEL VORTEX, WITH ADDITIONAL HOT TOWERS FLARING ON THE NORTHWEST SIDE, BEGINNING TO FORM A BANDING EYE TYPE FEATURE. HOWEVER, PREVIOUS ATTEMPTS TO WRAP THE CONVECTION UP THE EAST SIDE HAVE FAILED, SO IT REMAINS TO BE SEEN IF THIS ROUND WILL BE SUCCESSFUL. GFS AREA-AVERAGED SOUNDINGS INDICATE THE PRESENCE OF MODERATE EASTERLY SHEAR BELOW THE OUTFLOW LAYER AS WELL AS RELATIVELY DRY AIR IN THE MID- TO UPPER-LEVELS, WHICH WOULD SERVE TO HINDER SUSTAINED CONVECTIVE DEVELOPMENT AND SUSTAINMENT ON THE EASTERN SIDE OF THE CIRCULATION. A TIMELY 011728Z AMSR2 37GHZ IMAGE SHOWED A VERY WELL-DEFINED LOW LEVEL MICROWAVE EYE FEATURE, WHICH SUPPORTED THE INITIAL POSITION WITH HIGH CONFIDENCE. MEANWHILE THE 89GHZ IMAGE SHOWED A SOLID INNER EYEWALL, WITH FRAGMENTARY DEEP CONVECTION ON THE NORTHEAST SIDE, AND WHAT COULD BE THE INITIAL HINTS AT A SECONDARY EYEWALL ALREADY STARTING TO FORM TO THE SOUTH OF THE CENTER. THE INITIAL INTENSITY IS SET WITH MEDIUM CONFIDENCE BASED ON THE OVERALL AGREEMENT OF AVAILABLE SUBJECTIVE AND OBJECTIVE INTENSITY ESTIMATES. ENVIRONMENTAL ANALYSIS REVEALS FAVORABLE CONDITIONS, WITH LOW (10-15 KTS) EASTERLY WIND SHEAR, ROBUST RADIAL OUTFLOW AND AN ENHANCED EQUATORWARD OUTFLOW CHANNEL, AND ZESTY SSTS. THE SYSTEM IS CURRENTLY TRACKING TOWARDS THE NORTHWEST ALONG THE WESTERN SIDE OF A DEEP-LAYER SUBTROPICAL RIDGE (STR) CENTERED TO THE NORTHEAST. INITIAL WIND RADII BASIS: PERSISTENCE CURRENT STEERING MECHANISM: WESTERN PERIPHERY OF A DEEP-LAYER SUBTROPICAL RIDGE (STR). AGENCY DVORAK AND AUTOMATED FIXES: PGTW: T4.5 - 77 KTS RJTD: T4.0 - 65 KTS KNES: T4.5 - 77 KTS CIMSS SATCON: 82 KTS AT 011724Z CIMSS ADT: 84 KTS AT 011730Z FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: FAVORABLE VWS: 10-15 KTS SST: 30-31 CELSIUS OUTFLOW: STRONG RADIAL OTHER FACTORS: MODERATE MID-LEVEL SHEAR AND DRY AIR. 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: WHILE TY 14W HAS CONTINUED TO INTENSIFY OVER THE PAST SIX HOURS, THE PACE OF INTENSIFICATION HAS SLOWED AS THE SYSTEM CONTINUES TO SLOWLY CONSOLIDATE AND CONTINUES TO STRUGGLE A BIT AGAINST MODERATE MID- TO UPPER-LEVEL SHEAR AND A BIT OF DRY AIR IN THE MID-LEVELS. THE SYSTEM IS EXPECTED TO TRACK NORTHWESTWARD THROUGH THE NEXT 36 HOURS ALONG THE WEST SIDE OF A DEEP STR TO THE EAST. AROUND TAU 48, THE SYSTEM REACHES AN INFLECTION POINT WHEN THE RIDGE BUILDS IN ROUGHLY ALONG AN OKINAWA TO FUZHOU AXIS, AND THE TRACK SHIFTS OVER TO A MORE WESTWARD DIRECTION. BY TAU 72, THE SYSTEM WILL BE TRACKING WESTWARD TOWARDS THE SOUTHERN COAST OF TAIWAN, WITH LANDFALL ANTICIPATED ALONG THE FAR SOUTHERN PORTION OF TAIWAN SHORTLY AFTER TAU 72. THE SYSTEM IS EXPECTED TO SLOW DOWN AS IT APPROACHES TAIWAN, WITH POTENTIALLY SLOW, ERRATIC MOTION TO FOLLOW AFTER LANDFALL. THE SYSTEM IS FORECAST TO MOVE BACK OVER WATER TO THE WEST OF KAOHSIUNG BY TAU 96 THOUGH TRACK SPEEDS WILL BE QUITE SLOW AS IT CONTINUES TRACKING WEST THROUGH THE REMAINDER OF THE FORECAST PERIOD. IN TERMS OF INTENSITY, IF THE RECENT BURST OF CONVECTIVE ACTIVITY CAN SUSTAIN ITSELF AND WRAP AROUND THE CORE AND ESTABLISH AN EYE, INTENSITY ESTIMATES WILL RAPIDLY INCREASE. HOWEVER, THE PRESENCE OF DRY AIR AND MID-LEVEL SUB-OUTFLOW LAYER SHEAR IS EXPECTED TO HAVE A MAJOR ROLE IN KEEPING A LID ON THE INTENSIFICATION RATE. IN FACT, THE GFS, HAFS-A AND HWRF ALL SHOW AN INFLUX OF MORE DRY AIR FROM THE EAST, PARTICULARLY AFTER TAU 24, ALONG WITH INCREASED SHEAR AFTER TAU 48. THESE ARE LIKELY TO BE OFFSET BY THE STRONG RADIAL OUTFLOW AND THE INNER-CORE, ONCE ESTABLISHED, IS LIKELY TO BE ABLE TO FIGHT OFF THE SHEAR AND DRY AIR TO AN EXTENT. IN NET, THE SYSTEM IS STILL EXPECTED TO INTENSIFY, BUT AT A SLOW RATE, TO A PEAK OF 105 KNOTS BY TAU 48. AFTER PASSING TAIWAN AND BEING WEAKENED BY TERRAIN INFLUENCES, THE SYSTEM WILL CONTINUE TO WEAKEN IN THE SOUTHERN SECTION OF THE TAIWAN STRAIT DUE TO INCREASED SHEAR AND A REDUCTION IN UPPER-LEVEL OUTFLOW. MODEL DISCUSSION: THROUGH TAU 72, DETERMINISTIC MODELS ARE IN FAIRLY GOOD AGREEMENT, WITH THE EGRR MODEL NOW THE SOLE REMAINING OUTLIER ATTEMPTING TO TURN THE SYSTEM POLEWARD AFTER TAU 36. THE REMAINDER OF THE TRACKERS LIE WITHIN A 85NM ENVELOPE, CENTERED ON THE FAR SOUTHERN TIP OF TAIWAN. AFTER TAU 72, THE MODEL TRACKERS BEGIN TO DIVERGE, SPREADING OUT ALONG BOTH THE EAST-WEST AND NORTH-SOUTH AXES DUE TO DIFFERENCES IN HOW MUCH TERRAIN INTERACTION THE MODELS PREDICT. THE BULK OF THE GLOBAL MODELS SHOW THE SYSTEM CONTINUING TO MOVE FAIRLY QUICKLY TOWARDS THE WEST-SOUTHWEST, GENERALLY TOWARDS HONG KONG, WHILE THE MESOSCALE MODELS SHOW A MORE ERRATIC AND SLOW TRACK AFTER LANDFALL, KEEPING THE SYSTEM IN THE TAIWAN STRAIT THROUGH TAU 120. THE LATTER IS MORE LIKELY CONSIDERING THE COMPLEX TERRAIN INTERACTIONS AND ERRATIC MOTION THAT CAN BE EXPECTED FROM ANY TYPHOON MAKING LANDFALL ALONG THE SOUTHERN PORTION OF TAIWAN. THE JTWC FORECAST SLOWS DOWN AND PLACED NEAR THE MULTI-MODEL CONSENSUS, AND THUS LAGS FAR BEHIND THE FASTEST MODELS SUCH AS THE ECMWF AND GFS WHICH SUGGEST A POSITION SOUTH OF HONG KONG BY TAU 120. INTENSITY GUIDANCE IS MIXED, WITH A LARGE SPREAD IN POTENTIAL SCENARIOS, ROUGHLY BETWEEN 80 KNOTS AND 120 KNOTS. THE MORE AGGRESSIVE HWRF AND HAFS-A INDICATE THE SYSTEM GETTING UP TO 115 KNOTS OR SO BY TAU 24, WHICH IN THEORY IS POSSIBLE BUT SEEMS UNLIKELY DUE TO THE PRESENCE OF MID-LEVEL SHEAR AND DRY AIR. THE OTHER MODELS INCLUDED SHIPS AND THE GFS MESOSCALE SHOW A MUCH LOWER PEAK AT TAU 24 FOLLOWED BY STEADY WEAKENING THROUGH THE REMAINDER OF THE FORECAST. THE JTWC REACHES THE 105 KNOT PEAK OF THE CONSENSUS, BUT ABOUT 24 HOURS LATER, THEN FOLLOWS THE HAFS-A TRACKER AFTER TAU 72. CONFIDENCE IS LOW HOWEVER, THROUGH THE FORECAST PERIOD DUE TO THE LACK OF CONFIRMATION THAT THE SHEAR AND DRY AIR IS IN FACT THERE AND THE SUBSEQUENT IMPACTS ON THE INTENSIFICATION TREND THOSE FACTORS WILL HAVE. FORECAST CONFIDENCE: TRACK 0 - 72 HR: HIGH TRACK 72-120 HR: LOW INTENSITY 0 - 72 HR: LOW INTENSITY 72-120 HR: LOW// NNNN