摘要
分析了华南4~6月降水量的年际变化特征及华南4~6月旱、涝年的500hPa高度距平场的主要差异。结果表明,4~6降水存在2.5~3年的准周期变化和持续10年左右的阶段性变化特征。旱、涝年1~3月500hPa高度距平场的分布基本反位相,4~6月的距平场也存在明显的差异。综合结果表明,从冬季开始到次年6月,旱、涝年500hPa高度距平沿50°N纬圈的演变具有基本相反的过程。
This paper investigates the interannual variation features of April to June precipitationand main difference in 500hPa height anomaly between drought and flood years in South China。Results show that the rainfall has a quasi periodic(2.5 to 3 year)oscillation and a 10 year or sopersistent variation as an interval feature;in the dry and wet years,the January to March 500 hPaanomaly patterns are basically in anti-phase and the April to June patterns differ widely。Comprehensive analysis indicates that the evolution of 500 hPa height anomaly from winter to the follow-ing June follows a roughly opposite direction along the 50°N parallel in the two types of years。
出处
《南京气象学院学报》
CSCD
1994年第3期327-331,共5页
Journal of Nanjing Institute of Meteorology
基金
国家气象局部门重点项目
关键词
降水异常
环流特征
准周期变化
abnormal precipitation,circulation features,quasi-periodic variation,step variation