摘要
利用1881~2002年我国东北地区的月、季降水资料,采用历史曲线分析、功率谱分析、小波变换等方法,重点分析了松花江流域和辽河流域降水的长期变化规律.结果表明:松花江流域和辽河流域的降水都存在着明显的年代际变化,松花江流域降水以27~30年周期为主,辽河流域降水周期比松花江流域略长,大概为35~38年左右.根据降水自身演变规律及自回归方法预测的结果,估计未来5~10年,松花江流域仍将处于少雨期,辽河流域少雨期维持时间可能会稍长一些.
Study on the precipitation variation features for the valleys of the Songhuajiang and Liaohe rivers is undertaken by means of a trend analysis, power spectral method and wavelet transform in terms of the monthly and seasonal precipitation data from 1881 to 2002. Results indicate that a remarkable interdecadal variation is inherent in the precipitation of the target region, dominated by 27-30 (35-38) year periods for the rainfall in the Songhuajiang (Liaohe) valleys. Based on the evolution of the rainfall itself and auto-regression estimation it is inferred that the former (latter) will remain in a drier (a still longer rain-deficient) stage in 5-10 years to follow.
出处
《应用气象学报》
CSCD
北大核心
2005年第5期593-599,共7页
Journal of Applied Meteorological Science
基金
国家自然科学基金项目(40375025)
全国水资源综合规划专题研究"气候变化对中国水资源情势影响的综合分析"共同资助