THE AREA OF CONVECTION PREVIOUSLY LOCATED NEAR 23.9S 41.8E, IS NOW LOCATED NEAR 24.4S 43.8E, APPROXIMATELY 365 NM SOUTH-SOUTHWEST OF ANTANANARIVO, MADAGASCAR. ANIMATED ENHANCED INFRARED SATELLITE IMAGERY SHOWS A FULLY EXPOSED AND ELONGATED LOW-LEVEL CIRCULATION CENTER (LLCC) WITH DEEP CONVECTION SHEARED SOUTHEAST OF THE LLCC. A 232233Z AMSU-N MICROWAVE PASS CLEARLY SHOWS THE GROSS ELONGATION OF THE LLCC AND THE SIGNIFICANT DISPLACEMENT OF THE ASSOCIATED CONVECTION. UPPER-LEVEL ANALYSIS INDICATES THE SYSTEM IS SOUTH OF AND OPENING DISTANCE FROM THE RIDGE AXIS IN AN AREA OF MODERATE TO STRONG (20-30 KNOT) WESTERLY VERTICAL WIND SHEAR (VWS); HOWEVER, ANIMATED WATER VAPOR SATELLITE IMAGERY, SHOWS STRONG SOUTHEASTWARD OUTFLOW IS HELPING SUSTAIN THE WAYWARD CONVECTION. MAXIMUM SUSTAINED SURFACE WINDS ARE ESTIMATED AT 25 TO 30 KNOTS. MINIMUM SEA LEVEL PRESSURE IS ESTIMATED TO BE NEAR 1000 MB. IN VIEW OF THE HIGH VWS, THE POTENTIAL FOR THE DEVELOPMENT OF A SIGNIFICANT TROPICAL CYCLONE WITHIN THE NEXT 24 HOURS REMAINS LOW.
- JTWC + EUMETSAT + CIMSS
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