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。
This pattern of SSTA distribution is related to summer rainfall anomaly of North China by means of the tropical convection activity and general circulation in the middle and high latitude. iv.
这种海温异常分布型可通过夏季热带对流活动和中高纬大气环流与华北夏季降水异常产生联系。
Wang S W, Huang J B. 2006. The instability relationship between summer rainfall over North China and India[J]. Prog Nat Sci, 16(8):980-985.
王绍武， 黄建斌。 2006。 中国华北与印度夏季降水遥相关的不稳定性[J]。 自然科学进展， 16（8）：980-985。
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