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Long-term trends in flood discharges of the Ulster and Upper Fulda (Germany): a statistical review

机译:阿尔斯特河和上富尔达河洪灾的长期趋势(德国):一项统计回顾

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摘要

Intensifying processes in the hydrological cycle, induced by global warming, involve the danger of increasing flood discharges. Therefore, in the more recent past several large-scale studies on long-term trends within flood discharge datasets were conducted in Germany. The aim of this work is to supplement the existing findings with a focused, more detailed view on a region within the Central German Uplands as one of the flood generation areas. For this purpose, the catchments of Ulster and Upper Fulda in Eastern Hesse were chosen as study area. Datasets of three gauges, covering the period from 1961 to 2010 as well as datasets of five gauges from 1972 to 2010 were analyzed with statistical methods. Linear trends were calculated, verified and screened for change points. For selected time series, differences in long-term mean maximum discharges before and after these change points were examined with annual, semi-annual and monthly resolution. Results mainly showed upward, but non-significant trends. Most distinctive upward linear trends were detected in time series of the Ulster's gauges. Change point analysis yielded a characteristic clustering around 1977. The examination of the long-term flood regimes' dynamics, before and after a harmonized break between 1977 and 1978, revealed higher discharges for the sub-series after 1977, primarily during the winter half year. The results coincide with the findings of large-scale studies for Central, Western and Southern Germany in many ways. In particular long-term flow patterns in contiguous catchments bear a close resemblance to those of the Ulster and Fulda.
机译:由全球变暖引起的水文循环的加剧过程涉及增加洪水流量的危险。因此,最近在德国对洪水数据集内的长期趋势进行了几项大规模研究。这项工作的目的是用集中,更详细的视图补充德国中部高地作为洪灾发生区之一的区域,以补充现有发现。为此,选择了东黑森州的阿尔斯特和上富尔达流域作为研究区域。使用统计方法分析了涵盖1961年至2010年的三个量表的数据集以及1972年至2010年的五个量表的数据集。计算,验证并筛选线性趋势以查找变化点。对于选定的时间序列,使用年度,半年度和月度分辨率检查这些变化点之前和之后的长期平均最大排放量的差异。结果主要显示上升,但趋势不显着。在阿尔斯特(Ulster)仪表的时间序列中检测到最明显的上升线性趋势。变化点分析在1977年左右产生了一个特征性的聚类。对1977年至1978年之间的协调性断裂前后的长期洪水状况进行了研究,发现1977年之后该子系列的排水量较高,主要是在冬季半年期间。 。该结果在许多方面与德国中部,西部和南部的大规模研究结果相吻合。特别是连续流域的长期流态与阿尔斯特河和富尔达流域非常相似。

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