WDPN31 PGTW 021500 MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI// SUBJ/PROGNOSTIC REASONING FOR TROPICAL DEPRESSION 04W (CHOI-WAN) WARNING NR 016// RMKS// 1. FOR METEOROLOGISTS. 2. 6 HOUR SUMMARY AND ANALYSIS. TROPICAL DEPRESSION (TD) 04W (CHOI-WAN), LOCATED APPROXIMATELY 51 NM SOUTH-SOUTHWEST OF MANILA, PHILIPPINES, HAS TRACKED NORTHWESTWARD AT 09 KNOTS OVER THE PAST SIX HOURS. ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY AND ANIMATED RADAR DATA FROM PAGASA, SHOW THAT TD 04W HAS BECOME A BIT MORE ORGANIZED OVER THE PAST SIX HOURS, WITH THE RADAR DATA SHOWING THE NASCENT CONVECTIVE BANDING TO GOOD EFFECT. WHILE THE RADAR DATA IS FAIRLY CONCLUSIVE, THE SATELLITE DEPICTION STILL SHOWS A RATHER DISORGANIZED STRUCTURE, WITH MODERATE NORTHERLY VWS AND SOME MID-LEVEL DRY AIR INHIBITING CONVECTIVE DEVELOPMENT ON THE NORTH SIDE OF THE SYSTEM, WHILE A MASS OF FLARING CONVECTION HAS DEVELOPED TO THE WEST OVER THE SOUTH CHINA SEA. THE INITIAL POSITION, OVER THE SOUTHERN PORTION OF LUZON NEAR CALATAGAN, IS ASSESSED WITH HIGH CONFIDENCE BASED PRIMARILY ON THE WEAK SPIRAL BANDS EVIDENT IN THE ANIMATED RADAR DATA AND SURFACE OBSERVATIONS. THE INITIAL INTENSITY REMAINS SET AT 30 KTS, HEDGED SLIGHTLY LOWER THAN A DVORAK CURRENT INTENSITY ESTIMATE OF T2.5 (35 KTS) FROM RJTD DUE TO THE OVERALL LACK OF A DISTINCT CONVECTIVE CORE AND THE OVERALL DISORGANIZED NATURE OF THE CONVECTION. ENVIRONMENTAL CONDITIONS HAVE REMAINED WEAKLY FAVORABLE FOR ADDITIONAL DEVELOPMENT, CHARACTERIZED BY VERY WARM (30-31C) SSTS, GOOD EQUATORWARD AND WESTWARD OUTFLOW AND MODERATE (15-20 KT) VWS. THE UPPER-LEVEL TROUGH THAT HAS BEEN CLOSELY TRACKING THE LLCC HAS BEGUN TO DISSIPATE, BUT ITS EFFECTS ARE STILL SEEN IN THE DOWNWARD VERTICAL MOTION ON THE NORTHERN PORTION OF THE SYSTEM. TD 04W IS TRACKING NORTHWEST ALONG THE WESTERN PERIPHERY OF THE DEEP STR TO THE NORTHEAST. 3. FORECAST REASONING. A. THERE IS NO CHANGE TO THE FORECAST PHILOSOPHY SINCE THE PREVIOUS PROGNOSTIC REASONING MESSAGE. B. OVER THE NEXT 24 HOURS, TD 04W IS FORECAST TO CONTINUE TRACKING NORTHWESTWARD ALONG THE SOUTHWEST PERIPHERY OF THE STEERING RIDGE, SKIRTING THE WESTERN COAST OF LUZON. DURING THE SAME TIMEFRAME, THE AFOREMENTIONED UPPER-LEVEL TROUGH WILL DISSIPATE, ALLOWING FOR DEVELOPMENT OF DIFFLUENT EASTERLY FLOW ALOFT OVER TOP OF THE SYSTEM, LEADING TO A SHORT PERIOD OF INTENSIFICATION THOUGH TAU 24. THE SYSTEM IS EXPECTED TO REACH A PEAK INTENSITY OF 35 KTS BY TAU 12 UNDER THESE SLIGHTLY IMPROVED CONDITIONS. BY TAU 36 THE SYSTEM WILL HAVE ROUNDED THE RIDGE AXIS AND BEGIN ACCELERATING NORTHEASTWARD TO THE EAST OF TAIWAN. AS IT MOVES POLEWARD IT WILL ENCOUNTER STEADILY INCREASING VWS AND CONVERGENT UPPER-LEVEL FLOW ALONG THE SOUTH SIDE OF A 200MB ANTICYCLONE, LEADING TO STEADY WEAKENING AND ULTIMATE DISSIPATION NO LATER THAN TAU 72 AS THE SYSTEM NEARS THE SOUTHERN RYUKU ISLANDS. DYNAMIC MODEL GUIDANCE IS IN GOOD AGREEMENT THROUGH THE DURATION OF THE FORECAST, WITH A MAXIMUM CROSS-TRACK SPREAD OF 100 NM AT TAU 36 AS THE SYSTEM ROUNDS THE RIDGE AXIS. CONSISTENT WITH EXPECTATIONS FOR RECURVING SYSTEM, ALONG-TRACK SPREAD INCREASES STEADILY AFTER TAU 48 AS THE SYSTEM ACCELERATES NORTHEASTWARD. THE JTWC TRACK LIES ON THE WESTERN SIDE OF THE GUIDANCE ENVELOPE THROUGH THE DURATION OF THE FORECAST. SOME NEAR-TERM DEVIATION RIGHT OR LEFT OF THE FORECAST TRACK IS EXPECTED AS THE LLCC INTERACTS WITH THE SHORELINE OF WESTERN LUZON BUT CONFIDENCE IN THE OVERALL TRACK IS HIGH.// NNNN