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KINGRIC|2014-3-9 16:44
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本帖最後由 KINGRIC 於 2014-3-9 17:06 編輯
JTWC發布TCFA
補上報文... CDO大致已建立起來THE AREA OF CONVECTION PREVIOUSLY LOCATED NEAR 15.4S
169.2E, IS NOW LOCATED NEAR 15.4S 167.7E, APPROXIMATELY 420NM NORTH
OF NOUMEA, NEW CALEDONIA. ANIMATED MULTISPECTRAL SATELLITE IMAGERY
DEPICTS A CENTRAL DENSE OVERCAST (CDO) FEATURE BUILDING OVER THE LOW
LEVEL CIRCULATION CENTER (LLCC), WHILE CONVECTIVE BANDING HAS
STARTED TO FORM IN THE PERIPHERIES. A 090634Z SSMIS MICROWAVE IMAGE
DEPICTS IMPROVING STRUCTURE AS TIGHTLY CURVED CONVECTIVE BANDING HAS
BECOME APPARENT IN THE CDO FEATURE. UPPER LEVEL ANALYSIS REVEALS AN
IMPROVING ENVIRONMENT WITH GOOD EQUATORWARD OUTFLOW AND MODERATE (15
TO 20 KNOTS) VERTICAL WIND SHEAR. SEA SURFACE TEMPERATURES IN THE
REGION ARE ALSO FAVORABLE FOR DEVELOPMENT. DYNAMIC MODEL GUIDANCE IS
AGGRESSIVELY DEVELOPING THIS SYSTEM AS IT CONTINUES TO CONSOLIDATE.
MAXIMUM SUSTAINED SURFACE WINDS ARE ESTIMATED AT 25 TO 30 KNOTS.
MINIMUM SEA LEVEL PRESSURE IS ESTIMATED TO BE NEAR 1002 MB. DUE TO
THE IMPROVING STRUCTURE AND FAVORABLE ENVIRONMENT, THE POTENTIAL FOR
THE DEVELOPMENT OF A SIGNIFICANT TROPICAL CYCLONE WITHIN THE NEXT 24
HOURS IS NOW HIGH.
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