中国降水异常 rainfall anomaly in China
山西夏季降水异常 summer precipitation anomalies over shanxi province
降水异常区域特性 regional characteristic of summer precipitation anomalies
东北夏季降水异常 summer rainfall anomaly in northeast china
贵州夏季降水异常 Precipitation anomalies in Guizhou Summer
中国东部夏季降水异常 east china summer rainfall
秋季异常降水 autumn rainfall anomaly
There was consanguineous relationship between summer rainfall anomaly in North China and continual circulation anomaly from spring to summer .
华北夏季降水异常与从春到夏的持续环流异常密切相关。
参考来源 - 华北夏季旱涝发生的规律及其与北极海冰的相关分析TPNES precipitation anomalies is the highest in Northwest China, and the dry years are more than the wet years, whereas no the lasting dry years.
青藏高原东北侧区是西北地区降水异常最为敏感的区域，其少雨年的概率大于多雨年，但不存在持续少雨年。
参考来源 - 西北地区及其青藏高原东北侧降水的气候特征与影响因子分析Thereinto, double rainy season in the southeast of the Plateau is the most important component with biggest coverage for the distribution of precipitation anomaly over the Plateau.
其中东南部双雨季型是青藏高原年降水变率的最重要组成部分，在该区降水异常变化的空间尺度也较大。
参考来源 - 器测时期青藏高原降水时空变化规律探讨·2,447,543篇论文数据，部分数据来源于NoteExpress
这对东亚夏季年际降水异常具有一定的预测意义。
华北夏季降水异常与从春到夏的持续环流异常密切相关。
There was consanguineous relationship between summer rainfall anomaly in North China and continual circulation anomaly from spring to summer .
春季高原热力异常与我国春夏的气温、降水异常有较好的关系。
There are better relationships between the spring heat anomalies over the TP to the anomalies of China temperature and precipitation in spring and summer.
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