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本帖最後由 t02436 於 2014-6-9 22:16 編輯
JTWC TCFATHE AREA OF CONVECTION PREVIOUSLY LOCATED NEAR 15.7N 102.1W, IS
NOW LOCATED NEAR 15.9N 102.3W, APPROXIMATELY 215 NM SOUTHEAST OF
MANZANILLO, MEXICO. ANIMATED ENHANCED INFRARED SATELLITE IMAGERY
SHOWS THE SYSTEM HAS SLOWLY CONSOLIDATED WITH FORMATIVE BANDS
CONCENTRATED ALONG THE EASTERN SEMI-CIRCLE OF A PARTIALLY EXPOSED
LOW LEVEL CIRCULATION CENTER. UPPER-LEVEL ANALYSIS INDICATES THE
CYCLONE IS UNDERNEATH A RIDGE AXIS IN AN AREA OF LOW (05-10 KNOT)
VERTICAL WIND SHEAR AND STRONG SOUTEASTWARD OUTFLOW THAT IS
PROVIDING VENTILATION TO THE CONVECTION. ADDITIONALLY, ALONG-TRACK
SEA SURFACE TEMPERATURES, AT 30 DEGREES CELSIUS, ARE HIGHLY
CONDUCIVE FOR FURTHER DEVELOPMENT. MAXIMUM SUSTAINED SURFACE WINDS
ARE ESTIMATED AT 20 TO 25 KNOTS. MINIMUM SEA LEVEL PRESSURE IS
ESTIMATED TO BE NEAR 1005 MB. THE POTENTIAL FOR THE DEVELOPMENT OF A
SIGNIFICANT TROPICAL CYCLONE WITHIN THE NEXT 24 HOURS IS HIGH.
(t02436於2014.06.09 22:16補報文)
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