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霧峰追風者|2017-12-23 04:35
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本帖最後由 霧峰追風者 於 2017-12-23 04:45 編輯
JTWC 19Z評級Low,中心半裸。
(1) AN AREA OF CONVECTION (INVEST 93P) HAS PERSISTED NEAR
16.7S 174E, APPROXIMATELY 210 NM WEST-NORTHWEST OF NADI, FIJI.
ENHANCED INFRARED SATELLITE IMAGERY SHOWS A PARTIALLY EXPOSED LOW
LEVEL CIRCULATION CENTER (LLCC), WITH DEEP FLARING CONVECTION
SHEARED TO THE SOUTH OF THE LLCC. A 221836Z GMI 89GHZ MICROWAVE
IMAGE INDICATES LOW LEVEL STRUCTURE WRAPPING INTO THE EXPOSED LLCC,
AND FORMATIVE BANDING IN THE DEEP CONVECTION TO THE SOUTH. UPPER
LEVEL ANALYSIS REVEALS CONVECTION IS BEING SUPPORTED BY STRONG
OUTFLOW AND DIVERGENCE ALOFT. HOWEVER, 93P IS LOCATED IN AN AREA OF
MODERATE (15-25 KT) VERTICAL WIND SHEAR (VWS), BORDERING ON HIGH VWS
TO THE WEST AND SOUTH. SEA SURFACE TEMPERATURES AND OCEAN HEAT
CONTENT ARE MARGINALLY UNFAVORABLE FOR DEVELOPMENT, WITH ONLY A
SHALLOW LAYER OF 26-27 DEGREE CELSIUS WATER AROUND THE SYSTEM, AND
SSTS DECREASING RAPIDLY TO THE SOUTH. THE FSU CYCLONE PHASE SPACE
HAS 93P AS A BORDERLINE WARM CORE SYSTEM, LIKELY TO TRANSITION TO
COLD-CORE AS IT TRACKS SOUTHWARD. GLOBAL MODELS PREDICT SLIGHT
INTENSIFICATION IN THE NEAR TERM, WITH WEAKENING PROJECTED AFTER 1-2
DAYS AS THE SYSTEM MOVES TO THE SOUTHEAST. MAXIMUM SUSTAINED SURFACE
WINDS ARE ESTIMATED AT 23 TO 28 KNOTS. MINIMUM SEA LEVEL PRESSURE IS
ESTIMATED TO BE NEAR 1004 MB. THE POTENTIAL FOR THE DEVELOPMENT OF A
SIGNIFICANT TROPICAL CYCLONE WITHIN THE NEXT 24 HOURS IS LOW.
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