分析了2004年夏季东亚大气环流的主要特点及对我国天气与气候的影响。
The East Asia atmospheric circulation in the summer of 2004 as well as its impact on the climate and anomalous weather in China are analyzed.
作者也简要介绍了东亚及中国气候年代际变化的特征及其和太平洋海表温度异常的联系，并讨论了东亚大气环流异常在PDO形成中的可能作用。
Moreover, the interdecadal climate variabilities in East Asia and China are also reviewed and possible role of these variations in the PDO is also discussed.
而欧亚中高纬区大气环流春季异常对东亚区夏季大气环流和降水异常起着非常重要的作用。
Meanwhile, the anomaly of the atmospheric circulation over the high latitude Eurasia during spring is crucial to the summer monsoon circulation and precipitation over East Asia.
利用GCM（大气环流模式）完成的一系列改变青藏高原地形高度的数值试验说明，东亚季风气候变化非常敏感地响应于高原隆升。
Simulations of climate variables from General Circulation Models(GCMs)usually contain large deviation due to the low resolution, which makes it difficult for regional studies.
利用GCM（大气环流模式）完成的一系列改变青藏高原地形高度的数值试验说明，东亚季风气候变化非常敏感地响应于高原隆升。
Simulations of climate variables from General Circulation Models(GCMs)usually contain large deviation due to the low resolution, which makes it difficult for regional studies.
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