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Flash Flood Risk Assessment in Egypt

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Flash Floods in Egypt

Part of the book series: Advances in Science, Technology & Innovation ((ASTI))

Abstract

The subject of the flash flood risk assessment is an inclusive task that relies on the characteristics of the study area and the nature of previously recorded incidents. The Egyptian Nile Wadies (East Nile, and West Nile) are draining toward the highest population density and associated assets, while the Red Sea and Sinai wadies are draining toward high-density touristic compounds and scattered big cities and connecting roads. The existence of high urban densities and associated assets in the highest discharge locations (at wadies outfalls) without adequate consideration of wadi paths led to a considerable wadies encroachments and catastrophic recorded incidents. All recorded incidents are either due to unplanned urban and agricultural expansion, or insufficient flood mitigation measures, or lack of maintenance. Due to the freshwater stress in Egypt, the rainfall harvesting in the form of dams or artificial lakes should be considered as a top priority flood mitigation measure wherever applicable. The total capacity of all flood protection dams and artificial lakes all over Egypt is about 70 million m3 (MWRI 2016) that raises the potentiality for more similar measures to increase the rate of investment return from both flood mitigation and reduction in freshwater stress. The available data for this study were sufficient enough to calculate the catchments peak discharge and runoff volume. The 100 year return period was selected for the peak discharge calculations. Many thresholds have been tested for catchment delineation in order to obtain a reasonable number of catchments suitable for such a regional-scale study. The SRTM 90 × 90 DEM file was utilized as an input in the delineation procedure, with selected threshold was set to 50 km2. Due to the large variance of the catchments peak discharge and runoff volume, the box plot technique was employed to eliminate the ranking outlier values. The catchments were classified into five categories very high risk, high risk, moderate risk, low to moderate risk, and low risk. This categorization was done for the Peak Flow Standardized Risk Factor (PFSRF) and Runoff Volume Standardized Risk Factor (RVSRF) in order to prioritize the flood mitigation measures required for projects. The classification based on the runoff volume can guide the designer accounting for rain harvesting projects that would increase the rate of investment return from both flood mitigation and the reduction of freshwater stress. A two-dimensional HEC-RAS rainfall-runoff modeling is conducted for Ras Gharib city by using updated 30 × 30 DEM files to contain the manmade topographical modifications. The model was verified versus aerial photos for the 2016 incident. In order to assess the effectiveness of the newly constructed culvert (16 vents, 3 m × 3 m box culvert) with attached two dikes, another updated two-dimensional HEC-RAS rainfall-runoff model has been conducted and the results showed significant improvement in flood intensity values in Ras-Gharib city.

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Abbreviations

\({\text{A}}\) :

Catchment Area (km2)

ASRF:

Catchment Area Standardized Risk Factor

CN:

Curve Number

\(D\) :

Rainfall duration corresponding to the time step of calculations

\(D_{d}\) :

Drainage density

\(d\) :

Flow depth

DSRF:

Drainage Density Standardized Risk Factor

\({\text{FI}}\) :

Flood Intensity

\(F_{s}\) :

Stream frequency

FSRF:

Drainage Frequency Standardized Risk Factor

GIS:

Geographic Information System

IF:

Intensity Factor

L :

Longest flow path in (m)

LSRF:

Surface flow Length Standardized Risk Factor

MENA:

The Middle East and North Africa

MWRI:

Ministry of Water Resources and Irrigation

\(N_{u}\) :

Number of streams of order (U)

\(N_{u + 1}\) :

Number of streams of order (U + 1)

O&M:

Operation and Maintenance

PFSRF:

Peak Flow Standardized Risk Factor

\(R_{b}\) :

Bifurcation ratio

RVSRF:

Runoff Volume Standardized Risk Factor

\(S_{\text{l}}\) :

Slope of the longest flow path

\({\text{SRTM}}\) :

Shuttle Radar Topography Mission

SSRF:

Slope Standardized Risk Factor

TCSRF:

Time of Concentration Standardized Risk Factor

\(T_{c}\) :

Time of concentration in (min)

\(T_{L}\) :

Lag time

\(T_{p}\) :

Time to peak discharge

\({\text{TL}}_{s}\) :

Total length of streams (m)

\({\text{TN}}_{s}\) :

Total number of streams

\(U\) :

Stream orders according to (Horton 1945)

\(V\) :

Flow Velocity

WSRF:

Weighted Standardized Risk Factor

WMO:

World Meteorological Organization

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Correspondence to Ahmed M. Helmi .

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Helmi, A.M., Zohny, O. (2020). Flash Flood Risk Assessment in Egypt. In: Negm, A. (eds) Flash Floods in Egypt. Advances in Science, Technology & Innovation. Springer, Cham. https://doi.org/10.1007/978-3-030-29635-3_13

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