Skip to main navigation Skip to search Skip to main content

Reconstructing palaeoflood magnitude and frequency for flood hazard assessment in arid regions: The northern Judea Desert Streams, Israel

  • Rami Zituni
  • , Noam Greenbaum
  • , Naomi Porat
  • , Gerardo Benito
  • University of Haifa
  • Oranim Academic College of Education
  • Geological Survey of Israel
  • CSIC - National Museum of Natural Sciences

Research output: Contribution to journalArticlepeer-review

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.

Original languageEnglish
Article numbere70314
JournalEarth Surface Processes and Landforms
Volume51
Issue number6
DOIs
StatePublished - Jun 2026
Externally publishedYes

Bibliographical note

Publisher Copyright:
© 2026 John Wiley & Sons Ltd.

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

  1. SDG 15 - Life on Land
    SDG 15 Life on Land

Keywords

  • ephemeral streams
  • flood frequency analysis
  • flood magnitude
  • Judean Desert
  • palaeoflood hydrology
  • risk assessment

Fingerprint

Dive into the research topics of 'Reconstructing palaeoflood magnitude and frequency for flood hazard assessment in arid regions: The northern Judea Desert Streams, Israel'. Together they form a unique fingerprint.

Cite this