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首页> 外文期刊>Journal of hydrologic engineering >Spatiotemporal Complexity Analysis of Daily Precipitation in a Changing Environment in Heilongjiang Province, China
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Spatiotemporal Complexity Analysis of Daily Precipitation in a Changing Environment in Heilongjiang Province, China

机译:不断变化的环境中黑龙江省日降水量的时空复杂性分析

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Complexity analysis is an important tool for research on water resources. Although physical methods and quantitative detection are typically used to explore system complexity, this study uses a method combining probabilistic statistics with nonlinear science. The precipitation concentration index (CI), Mann-Kendall trend testing, probability density functions, and chaotic characteristic quantity are used to assess the spatiotemporal complexity of precipitation in Heilongjiang Province, China. The results show that the annual precipitation in Heilongjiang Province exhibits distinct spatial patterns; the highest values occurred at 128 degrees E, gradually diminishing toward the east and west. Maximum precipitation was recorded at Shangzhi station (646mm). A negative value of Z, an indicator of a precipitation trend, indicates a decreasing trend and a positive Z value indicates an increasing trend. In Yichun and Shangzhi, areas with greater precipitation, Z values were -1.21 and -4.88, respectively. In contrast, Z values were 3.02 and 0.93 in Qiqihar and Tailai, respectively, areas with lower precipitation. These findings indicate that precipitation differences between different regions have decreased, with the distribution becoming more uniform. Using ArcGIS to determine the chaotic characteristics of daily precipitation, values in the central and northeastern plains were high, whereas those in northwestern mountains were low. Maximum max values (3.456x10-3), an indicator of the degree of chaos, were obtained at the Yilan and Suifenhe stations, whereas the minimum value (9x10-5) was obtained at the Huma station. The authors analyze factors that influence the hydrological cycle in the study region by combining regional population and natural resource conditions. The results of this research will provide a reference for existing research and a theoretical basis for the scientific management of water resources in the region.
机译:复杂度分析是水资源研究的重要工具。尽管通常使用物理方法和定量检测来探索系统的复杂性,但本研究使用了将概率统计与非线性科学相结合的方法。利用降水集中指数(CI),Mann-Kendall趋势检验,概率密度函数和混沌特征量来评估黑龙江省降水的时空复杂性。结果表明,黑龙江省年降水量具有明显的空间格局。最高值出现在128度E处,向东和向西逐渐减小。尚志站(646mm)录得最大降水。 Z的负值(表示降水趋势)表示下降的趋势,Z值正表示表示趋势的增加。在降水量较大的宜春和尚志地区,Z值分别为-1.21和-4.88。相反,在齐齐哈尔和泰来降水量较低的地区,Z值分别为3.02和0.93。这些发现表明,不同地区之间的降水差异已经减小,分布变得更加均匀。使用ArcGIS确定每日降水的混沌特征,中部和东北平原的值较高,而西北山区的值较低。在宜兰站和Su芬河站获得了最大值最大值(3.456x10-3),该值指示了混乱程度,而在胡马站获得了最小值(9x10-5)。作者通过结合区域人口和自然资源条件来分析影响研究区域水文循环的因素。研究结果将为现有研究提供参考,为该地区水资源的科学管理提供理论依据。

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