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首页> 外文期刊>Journal of Hydrology >Probabilistic dependence between streamflow and hydroclimatic variables and the possible linkages to large-scale atmospheric circulation: A case study in Baden-Wiirttemberg, Southwest Germany
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Probabilistic dependence between streamflow and hydroclimatic variables and the possible linkages to large-scale atmospheric circulation: A case study in Baden-Wiirttemberg, Southwest Germany

机译:流流和液压素变量与大规模大气循环可能的概率依赖性:在德国西南部的巴登 - Wiirttemberg中的一个案例研究

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摘要

This study presents an investigation of probabilistic relationships between streamflow and hydroclimatic variables (including precipitation, temperature and soil moisture) and the potential links to large-scale atmospheric circulation over Baden-Wurttemberg, Southwest Germany. First, the joint dependence between seasonal streamflow and hydroclimatic variables was established by using copulas. On the basis of the joint dependence structure, we estimated the probabilities of hydrological droughts and prolonged high-streamflow events conditioned upon two different scenarios (high and low) of hydroclimatic variables for various seasons over the study area. The results indicate that both precipitation and soil moisture are positively related to the streamflow variation in Baden-Wiirttemberg for each season and strongly impact the likelihoods of hydrological droughts and high-streamflow events. Temperature tends to have less impact on the streamflow variation, and an inverse connection between streamflow and temperature is found in spring and summer. Then, the connections between streamflow variability and large-scale atmospheric circulation in summer and winter were explored by using composite analysis. Although the atmospheric circulation patterns vary in each season, it can be found that in summer high streamflow anomalies over Baden-Wiirttemberg are related to a cyclonic activity over central Europe while low streamflow anomalies are linked to anticyclonic patterns over western Ireland. The high streamflow anomalies in winter are strongly impacted by the westerlies that play an important role in favoring warm and moist airstreams from the Atlantic Ocean towards the study area, while an opposite atmospheric pattern is found for the years with low streamflow anomalies. The presented probabilistic methodology could also be applied in other regions worldwide.
机译:该研究提出了对流流和液压变量(包括沉淀,温度和土壤水分)之间的概率关系的调查,以及在德国西南部的巴登 - 符腾堡州大规模大气循环的潜在环节。首先,通过使用Copulas建立季节性流流和液压变量之间的关节依赖性。在联合依赖结构的基础上,我们估计水文干旱和延长的高流出事件的概率,调节了研究区域的各个季节的两种不同场景(高低)的液体变量。结果表明,沉淀和土壤水分都与每个季节的Baden-Wiirttemberg中的流流变呈正相关,强烈影响水文干旱和高流出事件的可能性。温度趋于对流流变化的影响较小,并且在春季和夏季发现流流和温度之间的逆连接。然后,通过使用复合分析探索了夏季和冬季流出变异性和大规模大气循环之间的连接。虽然大气循环模式在每个季节都有不同的变化,但可以发现,在夏季,巴登 - 威范顿的夏季高流出异常与中欧的旋风活动有关,而低流出异常与西爱尔兰的反曲调模式相关联。冬季的高流出异常受到威斯利亚的强烈影响,这些威斯莱斯在偏爱大西洋朝向研究区域的热情和潮湿的气流中发挥着重要作用,而这种多年来的氛围则具有低流出异常的多年。呈现的概率方法也可以应用于全球的其他地区。

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