综上，环流变化解释了春季发生在南极臭氧层的所有年际变化，Salby及其同事们写道。
Taken together, the two observed that circulation changes accounted for "virtually all" of the year-to-year changes in springtime Antarctic ozone, Salby and colleagues write.
因此，春季南半球环流异常可以作为长江中下游夏季旱涝主要短期气候预测因子。
Therefore, the spring sh circulation anomaly is one of important short-term climate predictors for summer rainfall over the Yangtze River Valley.
而亚洲热带大气环流的年际变化与华南春季风降水的变化关系不大。
Changes in the Asian tropical atmospheric circulation has little influence on the spring monsoon in South China according to this research.
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