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桜slime|2013-2-18 14:24
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本帖最後由 桜slime 於 2013-2-18 14:25 編輯
THE AREA OF CONVECTION PREVIOUSLY LOCATED NEAR 5.3N
136.9E, IS NOW LOCATED NEAR 5.7N 131.8E, APPROXIMATELY 195 NM WEST-
SOUTHWEST OF PALAU. ANIMATED MULTISPECTRAL SATELLITE IMAGERY SHOWS
AN IMPROVING LOW LEVEL CIRCULATION CENTER (LLCC) WITH WEAKLY DEFINED
FORMATIVE BANDS OF CONVECTION. A RECENT 180038Z ASCAT PASS INDICATED
IMPROVEMENT IN THE LOW LEVEL STRUCTURE, WITH 15 TO 20 KNOT WINDS
ALONG THE NORTHERN PERIPHERY. UPPER LEVEL ANALYSIS INDICATES THE
LLCC REMAINS TO THE SOUTH OF A DEEP LAYERED SUBTROPICAL RIDGE WHICH
IS CREATING MODERATE LEVELS OF DIVERGENCE ALOFT, IN ADDITION TO LOW
TO MODERATE LEVELS OF VERTICAL WIND SHEAR (10 TO 20 KNOTS). SEA
SURFACE TEMPERATURES IN THE VICINITY OF THE LLCC ARE BETWEEN 28 AND
30 DEGREES CELSIUS. MAXIMUM SUSTAINED SURFACE WINDS ARE ESTIMATED AT
15 TO 20 KNOTS. MINIMUM SEA LEVEL PRESSURE IS ESTIMATED TO BE NEAR
1004 MB. BASED ON THE IMPROVING LLCC STRUCTURE, THE POTENTIAL FOR
THE DEVELOPMENT OF A SIGNIFICANT TROPICAL CYCLONE WITHIN THE NEXT 24
HOURS IS UPGRADED TO MEDIUM.
MEDIUM了
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