
THE AREA OF CONVECTION PREVIOUSLY LOCATED NEAR 1.6N
108.6E, IS NOW LOCATED NEAR 1.1N 107.7E, APPROXIMATELY 231 NM EAST
OF SINGAPORE, MALAYSIA. ANIMATED VISUAL SATELLITE IMAGERY DEPICTS
MOSTLY FLARING CONVECTION WITH SOME MID-LEVEL TURNING. THE SYSTEM
APPEARS TO BE DISSIPATING IN NATURE AND MODELS HAVE CONTINUED TO
BACK OFF THE DEVELOPMENT OF THE SYSTEM. A 130240Z METOP-B ASCAT
IMAGE SHOWS STRAIGHT LINE FLOW DUE TO THE COLD SURGE EVENT IN THE
SOUTH CHINA SEA. THE DISTURBANCE IS CURRENTLY LOCATED IN AN
UNFAVORABLE ENVIRONMENT WITH HIGH WIND SHEAR (25-30 KNOTS), BUT HAS
GOOD DIVERGENCE ALOFT, AND WARM SEA SURFACE TEMPERATURES (28-30
CELSIUS). GLOBAL MODELS ARE MIXED AS TO HOW THE SYSTEM WILL TRACK
BUT INDICATE THAT THE MOST LIKELY SCENARIO WILL REMAIN IN THE
VICINITY OF THE MALAYSIA PENINSULA AND DRIFT WEST AS IT INTERACTS
WITH THE NORTHEASTERLY SURGE EVENT. MAXIMUM SUSTAINED SURFACE WINDS
ARE ESTIMATED AT 15 TO 20 KNOTS. MINIMUM SEA LEVEL PRESSURE IS
ESTIMATED TO BE NEAR 1006 MB. THE POTENTIAL FOR THE DEVELOPMENT OF A
SIGNIFICANT TROPICAL CYCLONE WITHIN THE NEXT 24 HOURS
REMAINS MEDIUM.