华北汛期降水量的多寡主要受其汛期大雨的频率和暴雨的贡献率影响。
The rainfall over North China during rainy seasons is mainly influenced by the heavy rain frequency and the excessively heavy rainfall contribution.
另外，闽南地区后汛期降水量与同期NINO西海区和黑潮海区的海温成正相关关系。
Otherwise, the normat correlation exists between the corresponding SST in west sea area of NINO and the Kuroshio and the summer rainfall in southern Fujian.
结果表明：广东省全年及前、后汛期的降水量变化存在2~7年、10年和30年左右的周期；
The result shows that there exist cycles of 2-7ys, 10a and 30a in precipitation of annual, Apr. -Jun.
结果表明：广东省全年及前、后汛期的降水量变化存在2~7年、10年和30年左右的周期；
The result shows that there exist cycles of 2-7ys, 10a and 30a in precipitation of annual, Apr. -Jun.
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