

AN AREA OF CONVECTION HAS PERSISTED NEAR 16.3S
51.7E, APPROXIMATELY 320 NM EAST-NORTHEAST OF ANTANANARIVO,
MADAGASCAR. ANIMATED MULTISPECTRAL SATELLITE IMAGERY REVEALS A
WELL DEFINED LOW LEVEL CIRCULATION CENTER (LLCC) WITH INCREASING
DEEP CONVECTION IN THE VICINITY. UPPER LEVEL ANALYSIS INDICATES
THE AREA IS UNDER LOW VERTICAL WIND SHEAR WITH EXCELLENT UPPER
LEVEL OUTFLOW IN BOTH POLEWARD AND EQUATORWARD DIRECTIONS. MAX-
IMUM SUSTAINED SURFACE WINDS ARE ESTIMATED AT 20 TO 25 KNOTS.
MINIMUM SEA LEVEL PRESSURE IS ESTIMATED TO BE NEAR 1004 MB. DUE
TO VERY FAVORABLE OUTFLOW AND WIND SHEAR ENVIRONMENTS, THE
POTENTIAL FOR THE DEVELOPMENT OF A SIGNIFICANT TROPICAL CYCLONE
WITHIN THE NEXT 24 HOURS IS POOR.
18/0830 UTC 16.3S 52.2E T1.0/1.0 99S -- South Indian Ocean
THE SYSTEM IS PRETTY SMALL BUT SEEMS TO BE GETTING BETTER ORGANIZED. FURTHERMORE, IN THE FUTURE LET SEE HOW IT WILL INTERACT WITH MADAGASCAR.