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Spatial and Temporal Variation of Annual Precipitation in a River of the Loess Plateau in China

机译:黄土高原地区河流年降水量的时空变化

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摘要

Empirical orthogonal function (EOF) decomposition and geostatistical (semivariogram) analysis are used to analyze the spatial and temporal patterns of annual precipitation in theWeihe basin based on the data from 1960 to 2011 at 30 national meteorological stations within and surrounding the Weihe basin area of the Loess Plateau in China. Then the Mann-Kendall method is used to discriminate the variation points of precipitation series at each station. The results show that, during the study period, there was an overall reduction in annual precipitation across the basin and there were two spatial patterns: increase in the northwest, decrease in southeast and increase in the west, decrease in east. Variation points in the annual precipitation series at eachmeteorological station in the basin were detected, and they occur earliest in the southeast and downstream, then progressively later in the northwest and upstream areas. These variations were most frequent during the 1970s and 1980s.The findings have significant implications for the variations research of runoff in the basin and formulate robust strategies to adapt to climate change and mitigate its effects.
机译:基于经验正交函数(EOF)分解和地统计(半变异函数)分析,基于1960-2011年渭河盆地内及周边30个国家气象站的数据,分析了渭河盆地年降水的时空格局。中国黄土高原。然后采用Mann-Kendall方法判别每个站点的降水序列变化点。结果表明,在研究期间,整个盆地的年降水量总体上减少了,并且有两种空间格局:西北增加,东南减少,西部增加,东部减少。在盆地的每个气象站都检测到年降水序列的变化点,这些变化点最早出现在东南和下游,然后逐渐出现在西北和上游地区。这些变化在1970年代和1980年代最为频繁。这些发现对流域径流变化研究具有重要意义,并制定了适应气候变化和减轻气候变化影响的强有力的策略。

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