老J認為消散了 取消評級
不過未來應該還是有重新評級的可能吧
(1) THE AREA OF CONVECTION PREVIOUSLY LOCATED NEAR 7.2N
151.0E, HAS DISSIPATED(消散) AND IS NO LONGER SUSPECT FOR THE DEVELOPMENT
OF A SIGNIFICANT TROPICAL CYCLONE IN THE NEXT 24 HOURS.
AN AREA OF CONVECTION HAS PERSISTED NEAR 6.3N 153.2E,
APPROXIMATELY 100 NM SOUTHEAST OF CHUUK. ANIMATED ENHANCED INFRARED
SATELLITE IMAGERY REVEALS A BROAD AND PARTIALLY EXPOSED LOW LEVEL
CIRCULATION CENTER (LLCC) WITH FLARING CONVECTION. A 221705Z SSMI
MICROWAVE IMAGE REVEALS A SLIGHT INCREASE IN STRUCTURE AS THE LLCC
HAS BECOME MORE CONSOLIDATED DESPITE THE CONVECTION REMAINING BROKEN
AND DISORGANIZED. UPPER-LEVEL ANALYSIS REVEALS A POOR ENVIRONMENT
CHARACTERIZED BY MODERATE TO STRONG (20 TO 30 KNOTS) VERTICAL WIND
SHEAR AND DIVERGENT OUTFLOW. SEA SURFACE TEMPERATURES IN THE AREA
ARE FAVORABLE FOR DEVELOPMENT. MAXIMUM SUSTAINED SURFACE WINDS ARE
ESTIMATED AT 10 TO 15 KNOTS. MINIMUM SEA LEVEL PRESSURE IS ESTIMATED
TO BE NEAR 1007 MB. THE POTENTIAL FOR THE DEVELOPMENT OF A
SIGNIFICANT TROPICAL CYCLONE WITHIN THE NEXT 24 HOURS IS LOW.
