Derek Etkin presented "Applications of 2D Surface flow Modeling in the New HEC-RAS Version 5.0" at the 2016 Association of State Floodplain Managers conference.
ASFPM 2016: Applications of 2D Surface flow Modeling in the New HEC-RAS Version 5.0
1. June 23, 2016
Applications of 2D Surface Flow
Modeling in the new HEC-RAS
Version 5.0
ASFPM Annual National Conference, Grand Rapids, MI
Concurrent Session G
Derek Etkin, P.E.
2. Contents
1. Overview of HEC-RAS prior to 2D capabilities
2. Introduction to 2D Surface Flow Modeling in version 5.0
3. Applications of HEC-RAS 2D capability
4. Advantages and Opportunities
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3. HEC-RAS Overview
3
Open channel flow freeware published by USACE
HEC-2 developed in 1966 (FORTRAN), HEC-RAS released in 1995
Generates flood profiles from 1D Open Channel Flow energy
and continuity equations
4. HEC-RAS Overview
Cross sections developed from survey and LiDAR using
HEC-GeoRAS, an extension in ArcMap
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flowto
5. HEC-RAS Overview
Inundation mapping generated from profile interpolated
between cross sections and intersected with terrain data
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Source: FEMA (2013) Federal Guidelines for Inundation Mapping of Flood Risks Associated with Dam Incidents and Failures (FEMA P-946)
6. HEC-RAS Overview – Steady State
1-D Steady Flow – constant discharge
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2
o f
( /A)Q h+ gA( - S + S )=0
x x
α
Q=VA
Momentum Continuity
Simulate single, peak discharge from hydrologic analysis
7. HEC-RAS Overview – Unsteady Flow
1-D Unsteady Flow – variable discharge and storage
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Simulate routed hydrograph, storage between cross sections
2
o f
( /A)Q Q hgA( ) 0S St x x
α
Q A+ =0
x t
Momentum Continuity
11. 2D Flow Areas in HEC-RAS 5.0
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2D Flow Areas can be added to geometry file like Storage Areas
Digital Terrain Map now integrated into HEC-RAS input files
2D Flow Area properties imported from Digital Terrain Map
13. 2D Flow Area Calculations
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Unstructured Mesh with Implicit Finite Volume solver
Hydraulic properties of computational cells (and faces)
pre-processed from Digital Terrain Map
Diffusion Wave or Full Momentum 2D Equations
Source: Brunner, G.W. (2014) Combined 1D and 2D Modeling with HEC-RAS Source: USACE (2016) HEC-RAS 2D Modeling User’s Manual (CPD-68A)
14. 2D Flow Area Calculations
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Pre-processed stage-storage for each cell
Cells do not have a “flat bottom” or single depth.
Cell Volume
15. 2D Flow Area Calculations
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Pre-processed cross section for each cell face from Terrain Map
Conveyance between cells defined by rating curves
Cell Face
16. 2D Flow Area Calculations
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High resolution Digital Terrain Map
Lower resolution computational mesh
17. 2D Flow Area Linkages
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2D Flow Areas can be linked to 1D Flow Reaches
1D Flow Reaches
Upstream
Downstream
Lateral Connections
Storage Areas or other 2D Flow Areas
External Boundary Condition
Normal Depth, Rating Curve, Stage or Flow time series
21. HEC-RAS 2D Riverine Applications
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Useful for riverine flow outside of well-defined, single channels:
Inter-connected or braided channels
Dam breach flood waves with unpredictable paths
26. HEC-RAS 2D Technical Advantages
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Implicit Finite Volume approach
Improved stability
Cells can start completely dry
More robust than finite element or finite difference
Allows for larger time steps than explicit methods
Unstructured Mesh Flexibility
Cells do not have flat bottom
Allows larger computational cells without loss of terrain details
Cells can be sized according to terrain features
27. HEC-RAS 2D Project Advantages
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Public Domain
No license fees
Large community of practitioners
Widely accepted as HEC product
Pre- and Post-processing in MAPPER (and GeoRAS)
Can easily integrate 2D Flow Areas into existing HEC-RAS
models
Update old 1D HEC-RAS models
No need to decide 1D or 2D when selecting modeling software
Can use for screening approach and where to focus detail
29. CHALLENGES
Some limited capacity for modeling structures
Can represent weirs, levees, and culverts
Cannot use full 1D bridge modeling capabilities
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30. CHALLENGES
Processing of map inundation, removing “islands”
from high resolution grid; cleaning up “Leaking”
Can use hydraulic connectivity plots
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31. CHALLENGES
Limited by quality of LiDAR/Raster…
Adding bathymetry to LiDAR for “pure” 2D Flow Area runs
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Careful selection of 1D reaches and orientation of cross sections that avoid overtopping.
Assumes that bifurcation is understood
Splits to well-defined channels
Areas outside of the main channel which may experience lateral inundation and provide peak attenuating storage of the floodwave.
Assume a single water surface elevation. No momentum simulation.
Beta released in May 2014
First Final version released in 2016
RAS Mapper is more integrated in version 5.0
Digital Terrain Map is easily generated from more widely available LiDAR sets
2D Flow Areas can be added and modified to the model geometry in the same GUI as always.
2D Flow Areas
Full Momentum (“Saint-Venant”)
Gravity, friction, hydrostatic pressure, acceleration: waves and detailed flow transitions and collision with objects
Good for rapid changes in elevation
vs. Diffusion Wave
Just gravity, friction, pressure
Interconnected braided channels = like the previous example
No need for defining each single 1D reach before running simulation.
Two small reservoirs in series and on the steep valley slopes above a large New England river.
We wanted to know how laterally the wave would spread based on the topographic data we had.
Two small reservoirs in series and on the steep valley slopes above a large New England river with development along the banks.
A large culvert can handle 50-yr flow (~100 cfs), but the dam break we simulated in a 1D simulation had peak flow of ~3000 cfs.
We wanted to know how laterally the wave would spread based on the topographic data we had. The quality of the LiDAR doesn’t show the structures in the flat area
Dam breach for a water supply reservoir outside of urban area. Another consultant made a 1D model with detailed structure information but also with cross sections not wide enough in some places. The peak WSELs appeared to cause flow splits.
Made this screening run using their breach hydrograph to identify places where there might be overtopping into adjacent areas; how much,
The screening simulation took us about 4 hours in total to pull together and helped us figure out an approach for updating the existing 1D model with a lateral connection to a 2D flow area that follows the overflow path
We’re still learning how to make the best of the mesh editing tools, such as the fixed Break Line Cell Spacing.
The orientation and location of the cell faces is important. Defines conveyance.
Still looking into developing tools in GIS or maybe SMS
Also, helpfulThe default inundation mapping uses a sloping water surface where the surface is interpolated between cell centers,
Unlike 1D cross sections, it is difficult to manually edit the geometry data in 2D Flow Areas. You are really bound to the LiDAR you have.
LiDAR of course doesn’t include bathymetry. There is a great tool that can use a 1D reach to carve out a channel in the Terrain (in MAPPER), but this is only for areas where you have already built a 1D model.
For “pure” 2D runs, there is a challenge representing structures and large/deep rivers, where the LiDAR doesn’t capture the conveyance of the channel.