{"title":"Reconstructing palaeoflood magnitude and frequency for flood hazard assessment in arid regions: The northern Judea Desert Streams, Israel","authors":"Rami Zituni, Noam Greenbaum, Naomi Porat, Gerardo Benito","doi":"10.1002/esp.70314","DOIUrl":null,"url":null,"abstract":"<p>Ephemeral streams in desert regions exhibit a high interannual hydrological variability dominated by short-lived flows and isolated extreme floods. Increase in settlements, land use intensity and infrastructures during the past 70 years in arid regions in general and in the study area in particular requires a probabilistic approach to Flood Frequency Analysis (FFA). This analysis is hampered by the scarcity of rainfall and discharge gauging stations, and by the high temporal variability of extreme events. Here, we apply advanced palaeoflood hydrology techniques to estimate the magnitude and frequency of floods to improve the quality and reliability of flood risk analysis for infrastructure design. The study focusses on two basins in the Northern Judean Desert: Nahal (N.) Darga ephemeral stream (70 km<sup>2</sup>) and Nahal Arugot (215 km<sup>2</sup>). The sedimentological evidence of past large floods in Nahal Darga (70 km<sup>2</sup>) consists of 17 flood events deposited over the last 1000 years with a maximum palaeo-discharge of 300 m<sup>3</sup> s<sup>−1</sup>. In Nahal Arugot (215 km<sup>2</sup>), the palaeoflood record comprises 36 flood events that extend over the last 400 years, recording a maximum flood discharge of 830 m<sup>3</sup> s<sup>−1</sup>. In comparison, the palaeoflood discharges were 1.8 and 1.6 times larger than the maximum measured floods. Nevertheless, these discharges did not exceed the regional envelope curve of the Judean Desert. The improved FFA caused an increase in the estimated flood discharges for all return periods; in Nahal Darga, the 100-year flood increased from 110 m<sup>3</sup> s<sup>−1</sup>, for the gauged record only, to 160 m<sup>3</sup> s<sup>−1</sup> (45%) for the combined records, and in Nahal Arugot from 660 m<sup>3</sup> s<sup>−1</sup> to 980 m<sup>3</sup> s<sup>−1</sup> (48%). The FFA for the systematic data only underestimated the frequency of the large floods because of their short and discontinuous records. The incorporation of the palaeoflood data into the dataset provided more solid values to the FFA, which significantly improved the reliability of risk assessment.</p>","PeriodicalId":11408,"journal":{"name":"Earth Surface Processes and Landforms","volume":"51 6","pages":""},"PeriodicalIF":2.8000,"publicationDate":"2026-06-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Earth Surface Processes and Landforms","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1002/esp.70314","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOGRAPHY, PHYSICAL","Score":null,"Total":0}
引用次数: 0
Abstract
Ephemeral streams in desert regions exhibit a high interannual hydrological variability dominated by short-lived flows and isolated extreme floods. Increase in settlements, land use intensity and infrastructures during the past 70 years in arid regions in general and in the study area in particular requires a probabilistic approach to Flood Frequency Analysis (FFA). This analysis is hampered by the scarcity of rainfall and discharge gauging stations, and by the high temporal variability of extreme events. Here, we apply advanced palaeoflood hydrology techniques to estimate the magnitude and frequency of floods to improve the quality and reliability of flood risk analysis for infrastructure design. The study focusses on two basins in the Northern Judean Desert: Nahal (N.) Darga ephemeral stream (70 km2) and Nahal Arugot (215 km2). The sedimentological evidence of past large floods in Nahal Darga (70 km2) consists of 17 flood events deposited over the last 1000 years with a maximum palaeo-discharge of 300 m3 s−1. In Nahal Arugot (215 km2), the palaeoflood record comprises 36 flood events that extend over the last 400 years, recording a maximum flood discharge of 830 m3 s−1. In comparison, the palaeoflood discharges were 1.8 and 1.6 times larger than the maximum measured floods. Nevertheless, these discharges did not exceed the regional envelope curve of the Judean Desert. The improved FFA caused an increase in the estimated flood discharges for all return periods; in Nahal Darga, the 100-year flood increased from 110 m3 s−1, for the gauged record only, to 160 m3 s−1 (45%) for the combined records, and in Nahal Arugot from 660 m3 s−1 to 980 m3 s−1 (48%). The FFA for the systematic data only underestimated the frequency of the large floods because of their short and discontinuous records. The incorporation of the palaeoflood data into the dataset provided more solid values to the FFA, which significantly improved the reliability of risk assessment.
沙漠地区的短期河流表现出较高的年际水文变异性,主要是短期流量和孤立的极端洪水。在过去的70年里,在干旱地区,特别是在研究区域,住区、土地利用强度和基础设施的增加需要一种概率方法来进行洪水频率分析。这种分析受到降雨和流量测量站缺乏以及极端事件的高时间变异性的阻碍。本文采用先进的古洪水水文技术估算洪水的震级和频率,以提高基础设施设计洪水风险分析的质量和可靠性。该研究集中在北朱迪亚沙漠的两个盆地:达尔加河(70平方公里)和纳哈尔阿鲁格河(215平方公里)。Nahal Darga (70 km2)过去大洪水的沉积学证据包括过去1000年来沉积的17次洪水事件,最大古流量为300 m3 s - 1。在Nahal Arugot(215平方公里),古洪水记录包括过去400年的36次洪水事件,记录的最大洪水流量为830 m3 s - 1。相比之下,古洪水流量是最大测量洪水的1.8倍和1.6倍。然而,这些排放并没有超过朱迪亚沙漠的区域包络曲线。经改善的FFA导致所有回潮期的估计洪流量增加;在纳哈尔达尔加,100年的洪水从仅测量记录的110 m3 s - 1增加到综合记录的160 m3 s - 1(45%),在纳哈尔阿鲁戈,从660 m3 s - 1增加到980 m3 s - 1(48%)。系统资料的FFA由于记录时间短且不连续,低估了大洪水发生的频率。将古洪水数据纳入数据集为FFA提供了更可靠的值,显著提高了风险评估的可靠性。
期刊介绍:
Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with:
the interactions between surface processes and landforms and landscapes;
that lead to physical, chemical and biological changes; and which in turn create;
current landscapes and the geological record of past landscapes.
Its focus is core to both physical geographical and geological communities, and also the wider geosciences