揭示了当赤道东印度洋海区的温跃层变浅时，温跃层反馈作用会加强，由此会引起IOD模态强度的增加和其他特征的改变。
With a shoaling of the EEIO thermocline, the thermocline feedback strengthens, and this leads to an increase in IOD variance and other characteristics changing.
揭示了当赤道东印度洋海区的温跃层变浅时，温跃层反馈作用会加强，由此会引起IOD模态强度的增加和其他特征的改变。
With a shoaling of the EEIO thermocline, the thermocline feedback strengthens, and this leads to an increase in IOD variance and other characteristics changing.
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