ABPW10 PGTW 200230 MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI// SUBJ/SIGNIFICANT TROPICAL WEATHER ADVISORY FOR THE WESTERN AND SOUTH PACIFIC OCEANS REISSUED/200230Z-200600ZDEC2024// REF/A/MSG/JOINT TYPHOON WRNCEN PEARL HARBOR HI/191821ZDEC2024// AMPN/REF A IS A TROPICAL CYCLONE FORMATION ALERT CANCELLATION.// RMKS/ 1. WESTERN NORTH PACIFIC AREA (180 TO MALAY PENINSULA): A. TROPICAL CYCLONE SUMMARY: NONE. B. TROPICAL DISTURBANCE SUMMARY: (1) THE AREA OF CONVECTION (INVEST 96W) PREVIOUSLY LOCATED NEAR 9.9N 125.7E IS NOW LOCATED NEAR 9.1N 123.6E, APPROXIMATELY 166 NM NORTHWEST OF DAVAO. ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY DEPICTS A BROAD AREA OF POORLY DEFINED CIRCULATION WITH THE LOW-LEVEL CIRCULATION CENTER BECOMING MORE FULLY EXPOSED WITH FLARING CURVED CONVECTIVE BANDS TO THE NORTH-NORTHEAST. FURTHERMORE, DRY AIR IS BEGINNING TO WRAP MORE INTO THE WEAKLY DEFINED LLCC. A 191200Z ASCAT METOP-B 25KM SCATTEROMETERY PASS REVEALS ASYMMETRIC GRADIENT INDUCED 20-25 KNOTS OF NORTHEASTERLY WIND ABOUT 100NM TO THE NORTHEAST. ENVIRONMENTAL ANALYSIS INDICATES THAT 96W IS IN A MARGINALLY FAVORABLE ENVIRONMENT FOR DEVELOPMENT DUE TO WARM (28-29C) SEA SURFACE TEMPERATURES, LOW (LESS THAN 15 KNOTS) VERTICAL WIND SHEAR, WHICH IS OFFSET BY WEAK EQUATORWARD OUTFLOW ALOFT. AS THE SYSTEM MOVES THROUGH THE BOHOL SEA, INTERACTION WITH COMPLEX TERRAIN FEATURES WILL FURTHER DISRUPT THE STRUCTURAL DEVELOPMENT OF THE CIRCULATION. GLOBAL MODELS ARE IN POOR AGREEMENT WITH 96W CONSOLIDATING OVER THE NEXT 24 HOURS. MAXIMUM SUSTAINED SURFACE WINDS ARE ESTIMATED AT 18 TO 23 KNOTS. MINIMUM SEA LEVEL PRESSURE IS ESTIMATED TO BE NEAR 1005 MB. THE POTENTIAL FOR THE DEVELOPMENT OF A SIGNIFICANT TROPICAL CYCLONE WITHIN THE NEXT 24 HOURS REMAINS LOW. SEE REF A (WTPN21 PGTW 191830) FOR FURTHER DETAILS. (2) NO OTHER SUSPECT AREAS. C. SUBTROPICAL SYSTEM SUMMARY: NONE. 2. SOUTH PACIFIC AREA (WEST COAST OF SOUTH AMERICA TO 135 EAST): A. TROPICAL CYCLONE SUMMARY: NONE. B. TROPICAL DISTURBANCE SUMMARY: (1) AN AREA OF CONVECTION (INVEST 96P) HAS PERSISTED NEAR 18.2S 144.1E, APPROXIMATELY 124 NM SOUTHWEST OF CAIRNS. ANIMATED MULTISPECTRAL SATELLITE IMAGERY (MSI) DEPICTS A BROAD ROTATION TO THE WEST OF TOWNSVILLE, AUSTRALIA, WHICH HAS STEADILY BUT SLOWLY CONSOLIDATED OVER THE PAST 12 HOURS. ANIMATED RADAR DATA SUGGESTS A TILTED VORTEX, WITH THE UPPER-LEVEL ROTATION PUSHING OUT TO THE SOUTHEAST OF THE LOW LEVEL CIRCULATION CENTER (LLCC). FLARING CONVECTIVE BANDS ARE EVIDENT IN THE EAST-SOUTHEASTERN PERIPHERY. A 191201Z ASCAT METOP-B SCATTEROMETERY PASS REVEALS ELEVATED 20-25 KNOT WINDS THAT ARE ALREADY PRESENT IN THE CORAL SEA, IN THE EASTERN EXTENT OF THE LARGER ROTATION. ENVIRONMENTAL ANALYSIS INDICATES THAT INVEST 96P IS IN A FAVORABLE AREA FOR FURTHER DEVELOPMENT WITH VERY WARM (30- 31C) SEA SURFACE TEMPERATURES, LOW (LESS THAN 15 KNOTS) VERTICAL WIND SHEAR, AND GOOD POLEWARD OUTFLOW ALOFT. GLOBAL MODELS ARE IN GOOD AGREEMENT THAT 96P WILL CONTINUE TO CONSOLIDATE OVER THE NEXT 24 HOURS AS IT MOVES SOUTHEASTWARD AND INTO THE CORAL SEA. THE POTENTIAL EXISTS FOR RAPID DEVELOPMENT ONCE THE SYSTEM EMERGES OVER THE WARM WATERS OF THE CORAL SEA. MAXIMUM SUSTAINED SURFACE WINDS ARE ESTIMATED AT 18 TO 23 KNOTS. MINIMUM SEA LEVEL PRESSURE IS ESTIMATED TO BE NEAR 1000 MB. THE POTENTIAL FOR THE DEVELOPMENT OF A SIGNIFICANT TROPICAL CYCLONE WITHIN THE NEXT 24 HOURS IS LOW. (2) NO OTHER SUSPECT AREAS. C. SUBTROPICAL SYSTEM SUMMARY: NONE. 3. JUSTIFICATION FOR REISSUE: ADDED LOW AREA IN PARA. 2.B.(1).//// NNNN