ABIO10 PGTW 262100 MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI// SUBJ/SIGNIFICANT TROPICAL WEATHER ADVISORY FOR THE INDIAN OCEAN REISSUED/262100Z-271800ZNOV2024// REF/A/MSG/JOINT TYPHOON WRNCEN PEARL HARBOR HI/261951ZNOV2024// REF/B/MSG/JOINT TYPHOON WRNCEN PEARL HARBOR HI/262021ZNOV2024// NARR/REFS A AND B ARE TROPICAL CYCLONE FORMATION ALERTS.// RMKS/ 1. NORTH INDIAN OCEAN AREA (MALAY PENINSULA WEST TO COAST OF AFRICA): A. TROPICAL CYCLONE SUMMARY: NONE. B. TROPICAL DISTURBANCE SUMMARY: (1) THE AREA OF CONVECTION (INVEST 99B) PREVIOUSLY LOCATED NEAR 7.5N 82.7E IS NOW LOCATED NEAR 8.3N 82.4E, APPROXIMATELY 174 NM EAST- NORTHEAST OF COLOMBO, SRI LANKA. ANIMATED ENHANCED INFRARED SATELLITE IMAGERY (EIR), AS WELL AS A 261229Z 91GHZ SSMIS IMAGE, DEPICT CURVED DEEP CONVECTIVE BANDING CONSOLIDATING NORTH OF THE CIRCULATION. A PARTIAL 261508Z ASCAT METOP-B PASS INDICATES THE AREA OF CONVECTION HAS A SYMMETRICAL STRENGTHENING CIRCULATION WITH 30 KNOT WINDS ON THE EASTERN PERIPHERY OF THE CIRCULATION. ENVIRONMENTAL ANALYSIS INDICATES A FAVORABLE ENVIRONMENT FOR FURTHER DEVELOPMENT WITH GOOD UPPER-LEVEL DIVERGENCE, WARM SEA SURFACE TEMPERATURES (29-30C), SYMMETRIC 850 MB VORTICITY, AND LOW TO MODERATE UPPER LEVEL WIND SHEAR (15-20KTS). GLOBAL DETERMINISTIC MODELS ARE IN GOOD AGREEMENT THAT INVEST 99B WILL CONSOLIDATE AND STRENGTHEN OVER THE NEXT 24 HOURS. MAXIMUM SUSTAINED SURFACE WINDS ARE ESTIMATED AT 28 TO 33 KNOTS. MINIMUM SEA LEVEL PRESSURE IS ESTIMATED TO BE NEAR 998 MB. THE POTENTIAL FOR THE DEVELOPMENT OF A SIGNIFICANT TROPICAL CYCLONE WITHIN THE NEXT 24 HOURS REMAINS HIGH. SEE REF A (WTIO21 PGTW 262000) FOR FURTHER DETAILS. (2) NO OTHER SUSPECT AREAS. C. SUBTROPICAL SYSTEM SUMMARY: NONE. 2. SOUTH INDIAN OCEAN AREA (135E WEST TO COAST OF AFRICA): A. TROPICAL CYCLONE SUMMARY: NONE. B. TROPICAL DISTURBANCE SUMMARY: (1) THE AREA OF CONVECTION (INVEST 96S) PREVIOUSLY LOCATED NEAR 9.7S 93.5E IS NOW LOCATED NEAR 10.7S 92.7E, APPROXIMATELY 260 NM WEST NORTHWEST OF COCOS ISLANDS. ANIMATED ENHANCED INFRARED SATELLITE IMAGERY (EIR) SHOWS PERSISTENT DEEP CONVECTION DISPLACED SLIGHTLY TO THE SOUTHWEST OF A PARTIALLY OBSCURED LOW LEVEL CIRCULATION CENTER (LLCC). A 261601Z ASCAT METOP-C 25KM PARTIAL PASS INDICATES DEFINED AND STRENGTHENING CIRCULATION WITH STRONG 30-35KT WINDS IN THE SOUTHWEST QUADRANT OF THE CIRCULATION BUT STARTING TO WRAP UP THE WESTERN SIDE. A 261633Z GMI 37GHZ MICROWAVE IMAGE REVEALED A RATHER DISORGANIZED LLCC, WITH LOW-LEVEL BANDING FEATURES IN THE NORTHERN HEMISPHERE OF THE CIRCULATION, AND STRONGER, MORE CONVECTIVE BANDING TO THE SOUTH. THE ENVIRONMENT IS FAVORABLE FOR DEVELOPMENT WITH CONDUCIVE WARM SEA SURFACE TEMPERATURES AND A STRONG 850 MB VORTICITY VALUE, AS WELL AS ROBUST RADIAL DIVERGENCE ALOFT OFFSET BY MODERATE TO HIGH (20-25KT) VERTICAL WIND SHEAR. GLOBAL DETERMINISTIC MODELS ARE IN AGREEMENT THAT INVEST 96S WILL CONSOLIDATE AND DRIFT POLEWARD OVER THE NEXT 24 TO 48 HRS. THE POTENTIAL FOR THE DEVELOPMENT OF A SIGNIFICANT TROPICAL CYCLONE WITHIN THE NEXT 24 HOURS IS HIGH. MAXIMUM SUSTAINED SURFACE WINDS ARE ESTIMATED AT 28 TO 33 KNOTS. MINIMUM SEA LEVEL PRESSURE IS ESTIMATED TO BE NEAR 998 MB. THE POTENTIAL FOR THE DEVELOPMENT OF A SIGNIFICANT TROPICAL CYCLONE WITHIN THE NEXT 24 HOURS IS UPGRADED TO HIGH. SEE REF B (WTXS21 PGTW 262030) FOR FURTHER DETAILS. (2) NO OTHER SUSPECT AREAS. C. SUBTROPICAL SYSTEM SUMMARY: NONE. 3. JUSTIFICATION FOR REISSUE: UPGRADED AREAS IN PARA. 2.B.(1) TO HIGH// NNNN