其经向风分量与纬向风分量同等重要。
The meridional wind component and zonal wind component are same important.
ITF的年代际变化是：年代际信号取决于赤道太平洋纬向风应力的变化。
The decadal variation of ITF is that the decadal signal lies in the change of latitude-oriented wind stress in the Equator-Pacific region.
时间系数的突变分析表明纬向风在1967年发生了一次较明显的减弱突变；
Mutation analysis of the time coefficient shows that there was a pronounced weakening mutation of the zonal wind in 1967.
这种周期振荡现象与赤道平流层的纬向风的准两年周期振荡现象有很好的对应关系。
It is well correspond to zonal wind oscillation on low layer of the stratosphere over Equator.
这是由于全球变暖中对流层静力稳定度的增强，与IOD模态相关的纬向风异常减弱。
The zonal wind anomalies associated IOD are found to weaken, likely due to increased static stability of the troposphere from global warming.
热带太平洋SOTA年际循环的驱动者主要是山异常东亚季风所引起的赤道西太平洋纬向风的异常。
The interannual cycle of SOTA in the tropical Pacific is driven by zonal wind anomaly over the equator ial western Pacific which is caused mainly by anomalous East-Asian winter monsoon.
结果显示：纬向风应力有35、47和57个月周期的传播型振荡； 经向风应力有28和38个月周期的传播型振荡。
The results show that the oscillations of zonal wind stress have 35 47 57 months, the oscillations of meridional wind stress have 28 38 months.
结果显示：纬向风应力有35、47和57个月周期的传播型振荡； 经向风应力有28和38个月周期的传播型振荡。
The results show that the oscillations of zonal wind stress have 35 47 57 months, the oscillations of meridional wind stress have 28 38 months.
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