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Ahmed Adel Saleh
Using HEC-RAS 5.x to assess flash flood
risk in arid regions
National Water Research Center – Water Resources Research Institute
NorAhmed1@Gmail.com
FB| ahmed.a.saleh.965
Flood risk assessment studies
Goals / measurement
Repeat what was done
• Apply the solved example during/after this presentation
Find my faults, mistakes and shortages
• Write a short report/note
Fix my errors
• Propose solutions (a short report/note)
Upgrade my work
• Make a workshop
Contents
Overview on flash flood risk assessment
Overview on HEC-RAS 5.0
Main steps of flood risk assessment
Discussion
Quick application
Overview on flash flood risk assessment
• Assessing
• Mapping
Objectives
• Depth
• Velocity
Criteria
Approaches of flood risk assessment
0.00
0.50
1.00
1.50
2.00
2.50
3.00
Waterdepth∙floodvelocity
(m2/s)
Low
Moderate
High
Extreme
Thresholds of risk to life
Shabanikiya H,. Behavior of crossing flood on foot, associated risk factors and estimating a predictive model. Nat Hazards
Approaches of flood risk assessment
0
0.5
1
1.5
2
2.5
3
3.5
4
4.5
5
0 1 2 3 4 5 6 7 8
Depth(m)
Velocity (m/s)
Instabilityzone
Stabilityzone
Vehicles stability thresholds
Approaches of flood risk assessment
0
0.5
1
1.5
2
2.5
3
0 0.5 1 1.5 2 2.5 3
Waterdepth(m)
Water depth ∙ flood velocity (m2/s)
High
Moderate
Low
flood/ structures damaged relationship
Approaches of flood risk assessment
Flood vs. damage curves in complex land uses.
Flood Risk Assessment Using ArcGIS
Con("Water Depth x Water Velocity"< 0.75, 1, Con("Water Depth x Water Velocity"< 1.5, 2,Con("Water Depth x
Water Velocity"< 2.25, 3,4)))
Con((("depth" < 1.7282 - 0.2597 * "Velocity") | ("depth" > 5.0471 * "Velocity"- 7.8786)),1,Con((("depth" >
2.1049-0.2779 * "Velocity") | ("depth" < 3.4145 * "Velocity"- 6.3621)),3,2))
Con((("depth"<0.5) & ("Depth x Velocity"<0.5)),1,Con((("depth" > 2.0) | ("Depth x Velocity">2.0)),3,2))
Con(("Velocity">2.0),1,2)
Why 2D hydrodynamic modeling?
Solving Equations
Principals of conservation
Newton’s laws of motion
Navier-stokes equations
Full Saint Venant / Diffusion Wave Equations
Full Saint Venant or Diffusion Wave ?
2D Saint Venant Equations
These equations are the conservative form of the Saint-Venant equations
. The first one is the mass conservations equation while the two others ar
e the momentum for the fluid:
x and y are the directions of the Cartesian Coordinate System used, qx and qy ar
e the flow rate in the x and y directions, respectively, t is the time, h is the water le
vel, H is the depth of the water column and Fx and Fy are the volume forces in th
e x and y directions, respectively.
Analytical  Numerical
Calculation points in HEC-RAS
HEC-RAS 5.x GU interface
HEC-RAS 5.x GU interface
HEC-RAS 5.x GU interface
Enter /Edit Geometry data
Enter /Edit
Flow data
Compute /Edit
Analysis parameters
HEC-RAS 5.x GU interface
Building a 2D simulation model using
HEC-RAS 5.x
Define Projection
Define Projection
All inserted layers should be
with the same projection
Define morphological data
Add Web data
Add terrain data
Add Land use data
Select a shp file
Define flow area
Define flow area
Define flow area
Define flow area
20m X 20m
Define flow area
Downstream Boundary
Condition
Upstream Boundary
Condition
Define flow area – Boundary conditions
Define flow area – Boundary conditions
Define flow data – Boundary conditions
Define flow data- Upstream Boundary Condition
OM_MERKA_07
Using HEC-HMS
Define flow data- Upstream Boundary Condition
Define flow data- Upstream Boundary Condition
Define flow data- Downstream Boundary Condition
Find Contour line of 0m a.s.l
Define flow data- Downstream Boundary Condition
Run the model
Run the model
Review Results
The whole story
• Control the results display
• Enhance the result accuracy
• Assis the risk using ArcGIS
• Representing the buildings

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Using HEC-RAS to assess flash floods risk in arid regions