#6 Postby Chacor » Wed Jun 01, 2011 6:12 am
0600 UTC:
THE AREA OF CONVECTION PREVIOUSLY LOCATED NEAR 7.7N
139.2E, IS NOW LOCATED NEAR 8.6N 136.5E, APPROXIMATELY 135 NM
NORTHEAST OF PALAU. ANIMATED MULTISPECTRAL SATELLITE IMAGERY
DEPICTS A BROAD AND WEAK LOW LEVEL CIRCULATION CENTER (LLCC) WITH
THE CONVECTION SHEARED TO THE WEST. A 312334Z SSMIS MICROWAVE IMAGE
DEPICTS WEAK CONVECTIVE CURVATURE. UPPER LEVEL ANALYSIS INDICATES
THE SYSTEM IS LOCATED BENEATH THE SUBTROPICAL RIDGE AXIS IN AN AREA
OF DIVERGENCE ALOFT AND MODERATE VERTICAL WIND SHEAR. SEA SURFACE
TEMPERATURES ARE FAVORABLE FOR DEVELOPMENT. MAXIMUM SUSTAINED
SURFACE WINDS ARE ESTIMATED AT 10 TO 15 KNOTS. MINIMUM SEA LEVEL
PRESSURE IS ESTIMATED TO BE NEAR 1008 MB. THE POTENTIAL FOR THE
DEVELOPMENT OF A SIGNIFICANT TROPICAL CYCLONE WITHIN THE NEXT 24
HOURS REMAINS LOW.
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