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首页> 外文期刊>ournal of the Meteorological Society of Japan >An Intraseasonal Amplitude Modulation of the Short-term Tropical Disturbances over the Western Pacific
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An Intraseasonal Amplitude Modulation of the Short-term Tropical Disturbances over the Western Pacific

机译:西太平洋短期热带扰动的季节内振幅调制

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The intraseasonal change of the activities of the short-term tropical disturbances are investigated in terms of their amplitude modulation. It has been revealed that the amplitude modulation in the tropics bears a periodicity around 30 days. It was also found that the enhanced phase of the amplitude modulation is often accompanied by the clustered genesis and/or development of tropical cyclones. The space-time analysis of the amplitude modulation has shown that it consists of two characteristic modes. One is the eastward-propagating mode with tonal wavenumber 1. Another mode shows a westward propagation and zonal wavenumber 4 to 6 as a characteristic longitudinal scale. Both modes appear equally significant in leading to enhanced disturbance activity.The large-scale circulation changes associated with the intraseasonal amplitude modulation are also investigated referring to the modulation over the tropical western Pacific. The composite analysis has revealed that the lower tropospheric westerly and the upper-level easterly are enhanced at the time of the enhanced activity of the tropical disturbances. The horizontal distribution of the circulation anomalies indicates that an intrusion of the low-level westerlies into the western Pacific takes place at this stage from the equatorial Indian Ocean through the South China Sea. This intrusion is also accompanied by enhanced cross-equatorial southerlies over the Indonesian region. In the upper levels, the intensification of the mid-Pacific trough is observed at the same stage.
机译:研究了短期热带干扰活动的季节内变化及其幅度调制。已经发现,热带地区的振幅调制具有30天左右的周期性。还发现振幅调制的增强阶段通常伴随着热带气旋的成簇发生和/或发育。幅度调制的时空分析表明,它由两个特征模式组成。一种是向东传播的模式,其音调波数为1。另一种模式显示了向西传播的纬向波数为4至6,这是特征纵向尺度。两种模式在增强干扰活动方面都表现出同样显着的意义。还参考热带西太平洋的调制研究了与季节内振幅调制有关的大规模环流变化。综合分析表明,随着热带扰动活动的增强,对流层下部的西风和东风的较高水平得到了增强。环流异常的水平分布表明,从赤道印度洋到南海,现阶段低层西风侵入西太平洋。这种入侵还伴随着印尼地区越赤道南风的增强。在高层,在同一阶段观察到了中太平洋海槽的加剧。

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