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首页> 外文期刊>Gluckauf-Forschungshefte >Time-series analysis of the run-off hydrograph for the Elbe water level at Dresden
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Time-series analysis of the run-off hydrograph for the Elbe water level at Dresden

机译:德累斯顿易北河水位径流水位的时间序列分析

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摘要

The present paper seeks to examine the available information on flow-water levels in Bavaria and Baden-Wurttemberg, in the form of hydrograph fluctuations, on the basis of flow levels recorded in Saxony. Various time-series analysis methods were used in obtaining the measurement data on the Elbe water level at Dresden, which was the site selected for the investigation. Periodic fluctuations with wave lengths of 13.6, 9.7 and 6.8 years were identified using both spectral analysis and auto-correlation analysis. These wave results interfere with each other and overlap with the annual cycle. The underlying reasons for this periodicity are as yet unexplained, though a solar origin cannot be ruled out. Subsequent investigation of the high water levels of August 2002 showed that the 13.6 and 6.8-year periodicities overlapped at that particular time. This overlap led to the increase in amplitude and therefore constituted the reason for the flooding.
机译:本文力求以萨克森州记录的水位为基础,以水文波动的形式研究巴伐利亚和巴登-符腾堡州的水位信息。各种时间序列分析方法用于获得德累斯顿易北河水位的测量数据,德累斯顿是进行调查的地点。使用光谱分析和自相关分析,可以确定波长为13.6、9.7和6.8年的周期性波动。这些波动结果相互干扰,并与年度周期重叠。尽管不能排除太阳起源,但仍无法解释这种周期性的根本原因。随后对2002年8月的高水位进行的调查显示,13.6和6.8年的周期在那个特定时间重叠。这种重叠导致幅度增加,因此构成了泛滥的原因。

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