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.
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.
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.
赤道东太平洋海温异常和印度洋偶极子有协同作用。
So Equator East Pacific SSTA and the IOD have synergic effect.
赤道东太平洋海温异常和印度洋偶极子有协同作用。
So Equator East Pacific SSTA and the IOD have synergic effect.
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