THE AREA OF CONVECTION PREVIOUSLY LOCATED NEAR 16.5S
37.7E, IS NOW LOCATED NEAR 16.4S 38.4E, APPROXIMATELY 510 NM NORTH-
NORTHWEST OF ANTANANARIVO, MADAGASCAR. ANIMATED INFRARED (IR)
SATELLITE IMAGERY REVEALS FORMATIVE BANDING WRAPPING INTO A LOW
LEVEL CIRCULATION CENTER (LLCC) THAT IS LOCATED OVER MOZAMBIQUE.
THE LLCC IS TRACKING EASTWARD, HEADING TOWARD THE OPEN WATER OF THE
MOZAMBIQUE CHANNEL. THE IR AND TOTAL PRECIPITABLE WATER LOOPS
SUGGEST THAT TIGHT TURNING OVER THE CHANNEL MAY BE CONSOLIDATING
AND FORMING A NEW LLCC. UPPER LEVEL ANALYSIS INDICATES A POINT
SOURCE HAS DEVELOPED OVER THE SYSTEM, PROVIDING GOOD OUTFLOW.
VERTICAL WIND SHEAR (VWS) IS MODERATE (20 KNOTS). SEA SURFACE
TEMPERATURES REMAIN FAVORABLE FOR DEVELOPMENT AT 29 TO 30 DEGREES
CELSIUS. NUMERICAL MODELS INDICATE DEVELOPMENT IS LIKELY OVER THE
NEXT 48 HOURS. MAXIMUM SUSTAINED SURFACE WINDS ARE ESTIMATED AT 20
TO 25 KNOTS. MINIMUM SEA LEVEL PRESSURE IS ESTIMATED TO BE NEAR 1003
MB. DUE TO IMPROVED BANDING AND FAVORABLE CONDITIONS OVER THE
MOZAMBIQUE CHANNEL, THE POTENTIAL FOR THE DEVELOPMENT OF
A SIGNIFICANT TROPICAL CYCLONE WITHIN THE NEXT 24 HOURS IS UPGRADED
TO MEDIUM.
Image: Madagascar's coastline can be seen through the convection. -
Satellite Rapid Response System (SRRS)
- JTWC + Eumetsat + Satellite Rapid Response System
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