Spatial and Temporal Variation Characteristics of Precipitation in North Canal Basin From 1960 to 2016

J. Zou, Shiyan Wang, Liu Chang, W. Liang, Yan-liang Du, Jiang Zhi
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Abstract

The temporal and spatial variation characteristics of precipitation in the basin are obtained by analyzing the precipitation data from 1960 to 2016 in the North Canal. The results show that: (1) The annual precipitation in the North Canal Basin has a weak downward trend as a whole, and there are alternating rising and falling characteristics between years. Uneven distribution during the year, precipitation is mainly concentrated in June to August, the average precipitation during this period accounted for 72% of the year;(2)The spatial distribution of precipitation in the basin is generally the most precipitation in the middle reaches, followed by the upper mountainous areas and the lower plains; In the seasons, the precipitation in the upper reaches of the summer is higher than that in the lower plains, and the opposite is true in winter.(3)The precipitation variation of the Northern Canal Basin is obvious, and the mutation point appeared in 1996 in the mid-1990s. This time node is consistent with the large regional pattern change of the Haihe River Basin; The periodic analysis shows that there are three periods of "bump-dry" change in the North Canal watershed, and the six oscillations on the 8-17a time scale are the most stable and significant, and the first main period is 13a.
1960 - 2016年北运河流域降水时空变化特征
通过对北运河1960 - 2016年降水资料的分析,得出了流域降水的时空变化特征。结果表明:(1)北运河流域年降水量总体上呈弱下降趋势,年际间呈上升和下降交替变化特征;年内分布不均匀,降水主要集中在6 ~ 8月,这一时期的平均降水量占全年的72%;(2)流域降水的空间分布总体上以中游降水最多,其次是上游山区和下游平原;(3)运河北部流域降水变化明显,突变点出现在1996年90年代中期。该时间节点与海河流域区域格局的大变化相一致;周期分析表明,北运河流域存在3个“干包”变化周期,其中8-17a时间尺度上的6个振荡最稳定、最显著,第一个主周期为13a。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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