THE AREA OF CONVECTION PREVIOUSLY LOCATED NEAR 4.4N
148.4E, IS NOW LOCATED NEAR 3.0N 155.1E, APPROXIMATELY 320 NM
SOUTHEAST OF CHUUK. ANIMATED MULTISPECTRAL SATELLITE IMAGERY SHOWS
CURVED BANDING AROUND A DEVELOPING LOW LEVEL CIRCULATION CENTER
(LLCC). UPPER LEVEL ANALYSIS INDICATES THE SYSTEM IS LOCATED BENEATH
DIFFLUENCE ALOFT AND IN AN AREA OF LOW VERTICAL WIND SHEAR. AN
OBSERVATION IN THE VICINITY IS REPORTING HIGH SEA SURFACE
TEMPERATURES (SST) OF 29 DEGREES CELSIUS, FAVORABLE FOR DEVELOPMENT.
MAXIMUM SUSTAINED SURFACE WINDS ARE ESTIMATED AT 15 TO 20 KNOTS.
MINIMUM SEA LEVEL PRESSURE IS ESTIMATED TO BE NEAR 1008 MB. DUE TO
UPPER LEVEL DIFFLUENCE AND HIGH SST, THE POTENTIAL FOR THE
DEVELOPMENT OF A SIGNIFICANT TROPICAL CYCLONE WITHIN THE NEXT 24
HOURS IS UPGRADED TO FAIR.