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kibishi0515|2017-2-15 16:22
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一對流區域(追蹤編號90P)佇留於接近西經148.6度、南緯13.4度,即在波拉波拉島東北方481.5公里之海面上。
AN AREA OF CONVECTION (INVEST 90P) HAS PERSISTED NEAR 13.4S 148.6W, APPROXIMATELY 260 NM NORTHEAST OF BORA BORA.
多色階動態衛星雲圖及祖魯時間15日4時23分之SSMIS 91GHz微波掃描顯示,對流雲系自該系統東北側起零散分佈於其低層環流中心外緣;祖魯時間14日18時34分之METOP-B ASCAT風場掃描顯示一狹長低層環流中心伴隨30節的強風呈現於此系統東側,但該強風似非由系統環流所產生。
ANIMATED MULTISPECTRAL SATELLITE IMAGERY AND A 150423Z SSMIS 91GHZ MICROWAVE IMAGE SHOWS SCATTERED CONVECTION ALONG THE OUTER EDGE, PRIMARILY ON THE NORTHEAST SIDE, OF A LOW LEVEL CIRCULATION CENTER (LLCC). A 141834Z METOP-B ASCAT PARTIAL PASS SHOWS AN ELONGATED LLCC WITH 30 KNOT WINDS TO THE EAST OF THE DISTURBANCE, BUT THE WINDS DO NOT APPEAR TO BE WRAPPING INTO THE CIRCULATION AT THIS TIME.
擾動當前位於一複雜環境之中,系統週邊之海面溫度偏暖(約為28℃),垂直風切較低(5至10節),赤道向流出狀況尚可;但系統相當鄰近一位於其南側之高空槽,將成為發展阻礙之一。
THE DISTURBANCE IS CURRENTLY LOCATED IN A MIXED ENVIRONMENT, WITH WARM SEA SURFACE TEMPERATURES (AROUND 28 C), LOW VERTICAL WIND SHEAR (5- 10 KNOTS), AND MODERATE EQUATORWARD OUTFLOW. HOWEVER AN UPPER LEVEL TROUGH POSITIONED JUST TO THE SOUTH IS HINDERING DEVELOPMENT.
全球模式認為此系統將於接下來數天內快速發展,基本而言,預報中認為氣壓梯度將增加此系統之東側外圍風力,並以副熱帶系統之形式持續向東南方行進。預報之最大持續風速為10至15節、最低氣壓為1010百帕。
GLOBAL MODELS SHOW SOME INTENSIFICATION OVER THE NEXT SEVERAL DAYS, PRIMARILY GRADIENT INDUCED AND CONFINED TO THE EASTERN PERIPHERY. MODELS ALSO INDICATE THE DISTURBANCE WILL TRACK TOWARDS THE SOUTHEAST AS A SUBTROPICAL SYSTEM. MAXIMUM SUSTAINED SURFACE WINDS ARE ESTIMATED AT 10 TO 15 KNOTS. MINIMUM SEA LEVEL PRESSURE IS ESTIMATED TO BE NEAR 1010 MB.
此系統於未來24小時內發展為一顯著熱帶氣旋之可能性評級為低。
THE POTENTIAL FOR THE DEVELOPMENT OF A SIGNIFICANT TROPICAL CYCLONE WITHIN THE NEXT 24 HOURS IS LOW.
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