簽到天數: 3293 天 [LV.Master]伴壇終老
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t02436|2014-7-28 08:13
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本帖最後由 t02436 於 2014-7-28 08:16 編輯
降評Low
THE AREA OF CONVECTION PREVIOUSLY LOCATED NEAR 14.4N
134.5E, IS NOW LOCATED NEAR 16.5N 134.0E, APPROXIMATELY 555 NM NORTH
OF KOROR, PALAU. ANIMATED ENHANCED INFRARED SATELLITE IMAGERY DEPICTS
A BROAD AND ELONGATED LOW LEVEL CIRCULATION CENTER (LLCC) WITH
INCREASINGLY LINEAR CONVECTION STREAMING TO THE WEST-SOUTHWEST FROM
THE CENTER OF THE SYSTEM. A RECENT 271244Z ASCAT PASS SHOWS THE LLCC
IS ORIENTED EAST-NORTHEAST TO WEST-SOUTHWEST AND IS BROADLY DEFINED
WITH CENTRAL WINDS NEAR 10 TO 15 KNOTS. UPPER LEVEL ANALYSIS SHOWS A
MARGINALLY CONDUCIVE ENVIRONMENT WITH WESTERLY DIVERGENT OUTFLOW AND
MODERATE TO STRONG (20 TO 30 KNOTS) VERTICAL WIND SHEAR (VWS). SEA
SURFACE TEMPERATURES IN THE REGION ARE FAVORABLE FOR DEVELOPMENT.
MAXIMUM SUSTAINED SURFACE WINDS ARE ESTIMATED AT 10 TO 15 KNOTS.
MINIMUM SEA LEVEL PRESSURE IS ESTIMATED TO BE NEAR 1005 MB. DUE TO
THE DISORGANIZED CONVECTION AND THE BROAD NATURE OF THE LLCC, THE
POTENTIAL FOR THE DEVELOPMENT OF A SIGNIFICANT TROPICAL CYCLONE
WITHIN THE NEXT 24 HOURS IS DOWNGRADED TO LOW.
整體對流鬆散 還有待發展
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