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Study on Spatiotemporal Evolution Characteristics of Regional Annual Precipitation

机译:区域年降水量的时空演化特征研究

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The study of the temporal and spatial evolution of precipitation is of great importance for the efficient use of water resources. This paper examines the long series of precipitation in Henan province from 1959-2018. Innovative Trend Analysis (ITA) method and Mann-Kendall (MK) test were used to analyze the characteristics of precipitation trend changes. Mann-Kendall (MK) mutation test and the sliding T method were used to study the jump features of precipitation. Wavelet analysis of the cyclical characteristics of precipitation. The results show that the spatial distribution of precipitation in Henan Province is uneven, with a gradual increase from north to south. The precipitation of northern, central and southern regions showed a downward trend, while that of western regions showed an upward trend. Both the northern and southern regions experienced jump features in precipitation around 1975 and 2008, while the western region experienced jump features around 1962 and 1980, and the central region experienced jump features around 1980; There are 3.5 different scales of “abundance and depletion” in the northern, western and southern regions, with a first principal cycle of 28a, and 5.5 different scales of “abundance and depletion” in the central region, with a first principal cycle of 17a.
机译:对沉淀的时间和空间演化的研究对于有效利用水资源来说是非常重要的。本文从1959 - 2018年审查了河南省长期降水。创新趋势分析(ITA)方法和Mann-Kendall(MK)测试用于分析降水趋势变化的特点。 Mann-Kendall(MK)突变试验和滑动T方法用于研究沉淀的跳跃特征。小波分析沉淀的周期性特征。结果表明,河南省降水的空间分布是不平衡的,北向南逐渐增加。北部,中央和南部地区的沉淀表现出了下降的趋势,而西部地区的趋势表现出上升趋势。北部和南部地区均经历了1975年和2008年的降水量的跳跃特征,而西部地区经历过1962年和1980年的跳跃特征,中部地区经历了1980年左右的跳跃特征;北部,西部和南部地区有3.5种不同的“丰富和耗尽”,其中第一个主要周期为28A,中央区域的第一个主要循环为17A的第一个主要周期。

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