WXTLIST WMO=ABPW10 ABPW10 PGTW 221200 2009326 1206 MSGID/GENADMIN/NAVMARFCSTCEN PEARL HARBOR HI/JTWC// SUBJ/SIGNIFICANT TROPICAL WEATHER ADVISORY FOR THE WESTERN AND /SOUTH PACIFIC OCEANS REISSUED/221200Z-230600ZNOV2009// REF/A/MSG/NAVMARFCSTCEN PEARL HARBOR HI/220751ZNOV2009// REF/B/MSG/NAVMARFCSTCEN PEARL HARBOR HI/220951ZNOV2009// NARR/REF A IS A TROPICAL CYCLONE WARNING. REF B IS A TROPICAL /CYCLONE FORMATION ALERT.// RMKS/ 1. WESTERN NORTH PACIFIC AREA (180 TO MALAY PENINSULA): A. TROPICAL CYCLONE SUMMARY: (1) AT 220600Z, TROPICAL DEPRESSION 26W (TWENTYSIX) WAS LOCATED NEAR 7.5N 148.5E, APPROXIMATELY 410 NM SOUTHEAST OF GUAM, AND HAD TRACKED NORTH-NORTHWESTWARD AT 09 KNOTS OVER THE PAST SIX HOURS. MAXIMUM SUSTAINED SURFACE WINDS WERE ESTIMATED AT 30 KNOTS GUSTING TO 40 KNOTS. SEE REF A (WTPN31 PGTW 220900) FOR FURTHER DETAILS. (2) NO OTHER TROPICAL CYCLONES. B. TROPICAL DISTURBANCE SUMMARY: (1) THE AREA OF CONVECTION PREVIOUSLY LOCATED NEAR 7.8N 128.9E, IS NOW LOCATED NEAR 8.2N 128.2E, APPROXIMATELY 390 NM WEST OF PALAU. ANIMATED MULTISPECTRAL SATELLITE IMAGERY SHOWS CONTINUED CONSOLIDATION OF DEEP CONVECTION NEAR A WELL-DEFINED LOW LEVEL CIRCULATION CENTER (LLCC) AND A 220500Z AMSRE AQUA MICROWAVE IMAGE SHOWS MULTIPLE CONVECTIVE BANDS CONVERGING INTO THE SYSTEM CENTER. THE 220035Z ASCAT PASS ALSO REVEALS A SYMMETRIC LLCC WITH 20-KNOT WINDS. ENVIRONMENTAL ANALYSIS INDICATES THE SYSTEM IS IN AN AREA OF MINIMAL VERTICAL WIND SHEAR AND HAS DIVERGENT FLOW ALOFT. AN UPSTREAM MID-LATITUDE TROUGH IS ALSO STARTING TO PROVIDE INCREASED POLEWARD OUTFLOW. A CIRCLE WAS USED FOR THE TROPICAL CYCLONE FORMATION ALERT AREA TO CONVEY NEAR-TERM TRACK UNCERTAINTY DUE TO THE SYSTEM BEING IN A DUAL STEERING ENVIRONMENT. MAXIMUM SUSTAINED SURFACE WINDS ARE ESTIMATED AT 17 TO 22 KNOTS. MINIMUM SEA LEVEL PRESSURE IS ESTIMATED TO BE NEAR 1006 MB. GIVEN AN INCREASE IN CONVECTIVE CONSOLIDATION AND IMPROVING POLEWARD OUTFLOW, THE POTENTIAL FOR THE DEVELOPMENT OF A SIGNIFICANT TROPICAL CYCLONE WITHIN THE NEXT 24 HOURS IS UPGRADED TO GOOD. SEE REF B (WTPN21 PGTW 221000) FOR FURTHER DETAILS. (2) AN AREA OF CONVECTION HAS PERSISTED NEAR 3.7N 107.8E, APPROXIMATELY 285 NM EAST-NORTHEAST OF SINGAPORE. ANIMATED INFRARED IMAGERY SHOWS CYCLONIC TURNING OF DEEP CONVECTION OVER A LOOSELY- DEFINED LOW LEVEL CIRCULATION CENTER (LLCC). IN ADDITION, NORTHEASTERLY LOW-LEVEL WINDS CAUSED BY A COLD SURGE THROUGH THE SOUTH CHINA SEA ARE ENHANCING THE LOW-LEVEL VORTICITY IN THE AREA. HOWEVER, EASTERLY VERTICAL WIND SHEAR IS CURRENTLY UNFAVORABLE FOR DEVELOPMENT. NEVERTHELESS, AS THE WIND SHEAR RELAXES, THERE IS EVENTUAL DEVELOPMENT OF A DEPRESSION-STRENGTH CYCLONE BY THREE OF THE GLOBAL MODELS. MAXIMUM SUSTAINED SURFACE WINDS (NOT ASSOCIATED WITH THE STRONGER GRADIENT WINDS TO THE NORTH) ARE ESTIMATED AT 12 TO 17 KNOTS. MINIMUM SEA LEVEL PRESSURE IS ESTIMATED TO BE NEAR 1007 MB. THE POTENTIAL FOR THE DEVELOPMENT OF A SIGNIFICANT TROPICAL CYCLONE WITHIN THE NEXT 24 HOURS IS POOR. (3) NO OTHER SUSPECT AREAS. 2. SOUTH PACIFIC AREA (WEST COAST OF SOUTH AMERICA TO 135 EAST): A. TROPICAL CYCLONE SUMMARY: NONE. B. TROPICAL DISTURBANCE SUMMARY: NONE. 3. JUSTIFICATION FOR REISSUE: UPGRADED AREA IN PARA 1.B.(1) TO GOOD AND ADDED AREA IN PARA 1.B.(2) AS POOR.// WXTLIST: done