结果表明：印度洋海温偶极振荡异常，引起了大气环流的异常，影响了季风强度和雨带分布。

Results show that the IOD anomaly results in anomalous atmospheric circulation, which affects the distribution of the rain belt during rainy seasons in China and the East Asian monsoon.

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结果表明，热带印度洋海温主要存在两种空间分布型，即全海盆符号一致的单极和东、西部符号相反的偶极。

The results show that the spatial distributions of SSTA are characterized by monopole with the same anomalous signs in basin-scale and by dipole with the reverse signs in the western and eastern tio.

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模拟研究的结果表明，印度洋海温主要影响孟加拉湾、中南半岛、印尼、印度次大陆及中国大陆南部地区的气候变化。

The results indicate that the Indian Ocean SSTA would mainly influence the climates of Bengal, Indo-China, Indonesia, India and China.

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