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frintezza|2012-8-19 12:40
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顯示全部樓層
看看老J評為LOW的一報
AN AREA OF CONVECTION HAS PERSISTED NEAR 16.7N 151.6E,
APPROXIMATELY 440 NM EAST-NORTHEAST OF GUAM. RECENT ANIMATED
ENHANCED INFRARED SATELLITE IMAGERY SHOWS AN AREA OF BROADLY
TURNING, BUILDING CONVECTION OVER WHAT SEEMS TO BE AN AREA OF TIGHT
TROUGHING, AS INDICATED BY THE 181149Z ASCAT AND 181404Z OSCAT
PASSES. CURRENT DATA SUGGESTS NO EVIDENCE OF A LOW-LEVEL CIRCULATION
CENTER (LLCC) BUT PERHAPS RATHER A VERY STRONG MID-LEVEL
CIRCULATION. UPPER-LEVEL ANALYSIS INDICATES THE DISTURBANCE IS
LOCATED A COUPLE OF DEGREES POLEWARD OF THE NEAR EQUATORIAL RIDGE
AXIS UNDER MODERATE (15-20 KNOTS) VERTICAL WIND SHEAR. ANIMATED
WATER VAPOR IMAGERY SHOWS ENHANCED EASTWARD OUTFLOW INTO A TROPICAL
UPPER-TROPOSPHERIC TROUGH CELL POSITIONED FURTHER EAST, WHILE
EQUATORWARD OUTFLOW REMAINS FAIR. SEA SURFACE TEMPERATURES ARE
FAVORABLE FOR TROPICAL CYCLONE DEVELOPMENT RANGING FROM 27-29
DEGREES CELSIUS. MAXIMUM SUSTAINED SURFACE WINDS ARE ESTIMATED AT 10
TO 15 KNOTS. MINIMUM SEA LEVEL PRESSURE IS ESTIMATED TO BE NEAR 1009
MB. DUE TO A LACK OF EVIDENCE SUPPORTING THE EXISTENCE OF A LLCC,
THE POTENTIAL FOR THE DEVELOPMENT OF A SIGNIFICANT TROPICAL CYCLONE
WITHIN THE NEXT 24 HOURS IS LOW
老J說98W根本就沒有LLCC, 只是中層旋轉明顯
現時風切中等
但東面的TUTT為98W加強向東的輻散, 而向南的流出亦良好
就因為找不到LLCC, 老J才評為LOW
........
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