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首页> 外文期刊>Journal of hydrologic engineering >Diagnosis of Change in Structural Characteristics of Streamflow Series Based on Selection of Complexity Measurement Methods: Fenhe River Basin, China
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Diagnosis of Change in Structural Characteristics of Streamflow Series Based on Selection of Complexity Measurement Methods: Fenhe River Basin, China

机译:基于复杂度测量方法选择的径流序列结构特征变化诊断:中国F河流域

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摘要

The analysis of the effects of human activities and climate variability on the structural characteristics of streamflow series facilitates further exploring the regularity of streamflow change and revealing the process of hydrological cycle response. The principal goal of this study is to establish an analysis system to diagnose the change in structural characteristics of streamflow series via employing suitable complexity measurement methods for specific cases. Meanwhile, an application scope table has been built based on testing and comparing the logicality and antinoise robustness through using logistic mapping series, random series, white noise, and 1/f noise for five commonly used complexity measurement methods (approximate entropy, permutation entropy, sample entropy, fractal, and Lempel-Ziv). According to the application scope table, sample entropy is the most suitable method for this specific case. Moreover, the results illustrate that in the prechange period, the complexity of the streamflow series is 0.5176; in the postchange period, the complexity value is 0.3722 if the streamflow is only impacted by climate variability; and its value is 0.2571 if it is impacted by both human activities and climate variability. Climate variability reduces the complexity of streamflow series, and human activities intensify this reduction. A decrease of complexity indicates that the streamflow series becomes more stable and regular.
机译:对人类活动和气候变化对水流序列结构特征的影响进行分析有助于进一步探索水流变化的规律性并揭示水文循环响应的过程。这项研究的主要目标是建立一个分析系统,通过针对特定情况采用适当的复杂性测量方法来诊断水流序列的结构特征的变化。同时,通过对逻辑映射序列,随机序列,白噪声和1 / f噪声五个常用的复杂度测量方法(近似熵,置换熵,样本熵,分形和Lempel-Ziv)。根据应用范围表,样本熵是针对此特定情况的最合适方法。此外,结果表明,在预交换期间,流量序列的复杂度为0.5176;而在预交换期间,流量序列的复杂度为0。在变更后时期,如果流量仅受气候变化影响,则复杂度值为0.3722;如果受人类活动和气候多变性的影响,则其值为0.2571。气候变化减少了水流序列的复杂性,而人类活动加剧了这种减少。复杂度的降低表明流序列变得更加稳定和规则。

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