#4 Postby euro6208 » Tue Nov 12, 2013 12:18 am
THE AREA OF CONVECTION PREVIOUSLY LOCATED NEAR 7.2S 94.2E,
IS NOW LOCATED NEAR 8.3S 93.7E, APPROXIMATELY 294 NM NORTHWEST
OF COCOS ISLAND. ANIMATED INFRARED SATELLITE IMAGERY DEPICTS A
CONSOLIDATING LOW-LEVEL CIRCULATION CENTER (LLCC) WITH CURVED DEEP
CONVECTIVE BANDING, PRIMARILY OVER THE SOUTHERN SEMI-CIRCLE. A
112307Z SSMIS MICROWAVE IMAGE INDICATES IMPROVED STRUCTURE WITH DEEP
CONVECTIVE BANDING WRAPPING INTO THE SOUTHEASTERN QUADRANT OF THE
LLCC WITH WEAK BANDING OVER THE NORTHERN SEMI-CIRCLE. A 111457Z
ASCAT IMAGE DEPICTS A WELL DEFINED CIRCULATION WITH 20 TO 25 KNOT
WINDS ALONG THE SOUTHERN SEMI-CIRCLE AND WEAKER 10-15 KNOT WINDS
ACROSS THE NORTHERN SEMI-CIRCLE. UPPER-LEVEL ANALYSIS SHOWS A
MARGINAL ENVIRONMENT WITH WEAK TO MODERATE (10 TO 20 KNOTS) VERTICAL
WIND SHEAR OFFSET BY STRONG DIFFLUENCE ALOFT. MAXIMUM SUSTAINED
SURFACE WINDS ARE ESTIMATED AT 20 TO 25 KNOTS. MINIMUM SEA LEVEL
PRESSURE IS ESTIMATED TO BE NEAR 1005 MB. THE POTENTIAL FOR THE
DEVELOPMENT OF A SIGNIFICANT TROPICAL CYCLONE WITHIN THE NEXT 24
HOURS IS UPGRADED TO MEDIUM.
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