#3 Postby euro6208 » Mon Sep 10, 2012 10:16 am
THE AREA OF CONVECTION PREVIOUSLY LOCATED NEAR 30.6N
148.3E, IS NOW LOCATED NEAR 30.4N 145.7E, APPROXIMATELY 430 NM
SOUTHEAST OF TOKYO, JAPAN. ANIMATED ENHANCED INFRARED SATELLITE
IMAGERY DEPICTS A PARTIALLY EXPOSED LOW LEVEL CIRCULATION CENTER
(LLCC) WITH PERSISTENT DEEP CONVECTION OVER THE SOUTH QUADRANT. A
092323Z METOP-A IMAGE SHOWS A DEFINED LLCC WITH WEAK CONVECTIVE
BANDING OVER THE SOUTHWEST QUADRANT WRAPPING INTO THE SOUTHEAST
QUADRANT. A 092322Z ASCAT IMAGE INDICATES A SMALL, DEVELOPING LLCC
WITH 15-20 KNOT WINDS AND ISOLATED 20-25 KNOT WINDS DISPLACED NORTH
OF THE CENTER; THESE STRONGER WINDS HAVE NOT YET WRAPPED INTO THE
LLCC. UPPER-LEVEL ANALYSIS INDICATES THAT THE LLCC IS LOCATED ALONG
THE NORTHERN EDGE OF A BROAD UPPER-LEVEL LOW AND IS UNDER MODERATE
(10-20 KNOTS) NORTHEASTERLY VERTICAL WIND SHEAR, WHICH IS HINDERING
CONVECTIVE ORGANIZATION. ADDITIONALLY, THERE IS ANOTHER WEAK,
BROAD, EXPOSED CIRCULATION EVIDENT TO THE SOUTHWEST AT 26.0N
144.4E. BASED ON THE DEFINED CIRCULATION EVIDENT ON THE RECENT
ASCAT IMAGE, MAXIMUM SUSTAINED SURFACE WINDS ARE ESTIMATED AT 12 TO
18 KNOTS. MINIMUM SEA LEVEL PRESSURE IS ESTIMATED TO BE NEAR 1006
MB. THE POTENTIAL FOR THE DEVELOPMENT OF A SIGNIFICANT TROPICAL
CYCLONE WITHIN THE NEXT 24 HOURS REMAINS MEDIUM.
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