Abstract

The Wadi Degla basin is amongst the most important basins in the north-eastern part of the Eastern Desert, east of Maadi, Cairo, which drains into River Nile. It covers an area of about 177.6 km2. Although it located in an arid region, the basin could receive a huge amount of rainwater during heavy rainstorms which in turn lead to initiate flash flood hazard and causing catastrophic effects on existing infrastructure of main gate and tracks of protected area, also threatened visitor's life and surrounding environments. The present study aims to evaluate of flash flood risk in Wadi Degla and possible mitigation. The morphometric parameters investigation were carried out using ASTER Digital Elevation Model (DEM), GIS, and geomorphic field observations. Using a technique given by El-Shamy, the risk degree for the Wadi Degla basin's vulnerability to flash flooding risk was calculated. The first technique focuses on the relationship between drainage density and bifurcation ratio, whereas the second relies on the relationship between drainage frequency and bifurcation ratio. For the examined basin of the watershed, the third morphometric parameter (the bifurcation ratio, drainage density, and stream frequency) were obtained and calculated. The bifurcation ratio, stream frequency, and drainage density all have values of 1.7, 6.05, and 2 according to morphometric study. The bifurcation ratio, stream frequency, and drainage density have morphometric values of 1.7, 6.05, and 2 respectively, as per morphometric analysis. The Wadi Degla has elongated shape. According to the computed metrics (e.g., stream frequency, bifurcation ratio and drainage density), the Wadi Degla basin catchment area falls into category (A). This means that there is expected high susceptibility of flash flooding possibility in the area under consideration. This expected risk leads the Ministry of Water Resources and Irrigation to establish three dams on the pass of Wadi Degla to work as an obstacle for decrease the flash flood velocity flow. Consequently, from an environmental hazards point of view, the Wadi Degla Protected Area should be closed during heavy rainfall for visitor safety and also avoid the establishment of any basic infrastructure in the vicinity of the Wadi pass.

Highlights

  • The world is witnessing a recent climate change event, in particular the rise of temperature and heavy rain in locations that were not previously witnessed, and Egypt is one of those countries that are located in the dry regions, but the past twenty years have witnessed change and precipitation and the occurrence of flash floods that led to the destruction of the Basic structure and roads

  • Abdel Galil Abdel Hamid Hewaidy et al.: Flash Flood Risk Assessment of Wadi Degla Basin Protected Area, East of Maadi, Cairo, Egypt Based on Morphometric Analysis Using Geographic information systems (GIS) Techniques climate change has an impact on the frequency and magnitude of flash floods. [1]

  • As a result of the plot of stream frequency vs bifurcation ratio, the Wadi Degla catchment region is classified as Zone A, suggesting a high risk of flash flooding

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Summary

Introduction

The world is witnessing a recent climate change event, in particular the rise of temperature and heavy rain in locations that were not previously witnessed, and Egypt is one of those countries that are located in the dry regions, but the past twenty years have witnessed change and precipitation and the occurrence of flash floods that led to the destruction of the Basic structure and roads. On the 24th and 25th of April 2018, a strong rainstorm caused flash flooding in the study region, with rainfall totals of 31.3 in Wadi Degla [20]. This flood has severely harmed the infrastructure in the Wadi Degla protectorate, where runoff water has filled most of gate facilities, parking area and remove signposts and visitor tracks. The purpose of this study is to apply GIS techniques to identify the potential flood hazard of Wadi Degla based on combining values of different geomorphic parameters and to estimate the degree of risk and to mitigate from this hazard

Site Description
Methodology
Linear Morphometric Parameters
Areal Aspect Morphometric Parameters
Relief Aspect
Flash Flood Risk Assessment
Conclusion and Recommendations
Full Text
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