In this paper, the seasonal changes of atmospheric circulation in the Northern Hemisphere induced by persistent anomaly of Arctic sea ice have bean examined.
本文利用全球9层15波谱模式，模拟了北极海冰后退期持续异常对北半球大气环流季节变化的影响。
In this paper, the seasonal changes of atmospheric circulation in the Northern Hemisphere induced by persistent anomaly of Arctic sea ice have bean examined.
本文利用全球9层15波谱模式，模拟了北极海冰后退期持续异常对北半球大气环流季节变化的影响。
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