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.
降水低频振荡呈现明显的由南向北的经向传播。
The low frequency oscillation of monsoon rainfall propagate in meridional direction from the south to the north.
一个有趣的特征是这一分量不是纬向波型的振荡而是经向波型的振荡。
An interesting feature is that this component is not a zonal wave type oscillation, but rather a meridional wave type fluctuation.
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