高密度云导风资料所揭示的发展和不发展热带气旋的对流层上部环流特征
DEVELOPING AND NON-DEVELOPING TROPICAL CYCLONES REVEALED BY HIGH DENSITY CLOUD MOTION WINDS
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摘要: 国家卫星气象中心建立了一套云导风计算的算法。自1997年以来,国家卫星气象中心使用该算法,利用GMS-5卫星的数据计算出西北太平洋上的1.25经纬度网格的卫星云导风。利用这套资料,对西北太平洋热带气旋发展的问题进行了研究。 通过研究发现,热带气旋通常是由对流层上层的西风急流引发的,那些西风急流可能是由深入到热带的中纬度槽所引起的,在盛夏季节,吹向热带对流层上部槽(TUTT)赤道一侧的西风也有可能引发台风。Abstract: It has been indicated by many authors that tropical cyclones with easterly in upper troposphere have less probability of development, while tropical cyclones with multidirectional outflow in upper troposphere have more probability of development. National Satellite Meteorological Center of China developed an algorithm of cloud motion wind calculation. This algorithm has an advantage of calculation amount saving. With this algorithm, cloud motion winds with grid length 1.25 degree lat/lon have been calculated since Oct. 1996 by using GMS-5 data in the North West Pacific region. The development perspective of tropical cyclones in the North West Pacific was examined. It was found that tropical cyclones were usually initiated by westerly jets in upper troposphere. Those westerly jets may be supplied by middle latitude troughs that deeply invade into the tropics. In mid-summer season those westerly jets may be supplied by westerly to the equatorial side of TUTT. It is concluded that cloud motion winds with high density are useful in diagnosing tropical cyclone development perspective in operation.
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Key words:
- Cloud motion winds /
- tropical cyclones /
- developing /
- westerly jets /
- middle latitude troughs /
- TUTT
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