This page reports on the performance of the Tygron Platform's Water Module by means of the UK EA Benchmark Test 4 – Speed of flood propagation over an extended floodplain.
The objective of this test is to assess the package’s ability to simulate the celerity of propagation of a flood wave and predict transient velocities and depths at the leading edge of the advancing flood front. It is relevant to fluvial and coastal inundation resulting from breached embankments.[1]
Description
This test is designed to simulate the rate of flood wave propagation over a 1,000 x 2,000 m floodplain following a defence failure (Fig. (a)). The floodplain surface is horizontal, at datum (= 0 m). One inflow boundary condition will be used, simulating the failure of an embankment by breaching or overtopping, with a peak flow of 20 m3/s and time base of ~6 h. The boundary condition is applied along a 20-m line in the middle of the western side of the floodplain.[1]
Figure (a): Modelled domain and the locations of the 20-m line of inflow, 6 output points, and the aimed for 0.1-m and 0.2-m contour lines at t = 1 h (dashed) and t = 3 h (solid), respectively.Animation of the test result for case 4, generated by the Tygron Platform. Map dimensions = 1,000 x 2,000 m. Grid-cell size = 5 m.Figure (b): Hydrograph applied as inflow boundary condition.
Boundary and initial condition
Inflow boundary condition as shown in Fig. (b)
All other boundaries are closed
Initial condition: dry bed
Parameter values
Manning’s n: 0.05 (uniform)
Model grid resolution (m): 5 (or ~80,000 nodes in the area modelled)
Simulated time (h): 5
Required output
Software package used: version and numerical scheme.
Specification of hardware used to undertake the simulation: processor type and speed, RAM.
Minimum recommended hardware specification for a simulation of this type.
Time increment used, grid resolution (or number of nodes in area modelled) and total simulation time to specified time of end.
Raster grids (or TIN) at the model resolution consisting of:
Depths at times 30mins, 1 hour, 2 hours 3 hours, 4 hours.
Velocities (scalar) at times 30mins, 1 hour, 2 hours 3 hours, 4 hours.
Plots of velocity and water elevation versus time (suggested output frequency 20s) at the six locations represented in Figure (a) and provided as part of dataset.
These locations are:
Point ID
X
Y
1
50
1000
2
100
1000
3
200
1000
4
300
1000
5
300
1000
6
300
1300
Dataset content
Upstream boundary condition table (inflow vs. time). Filename: Test4BC.csv
Location of output points. Filename: Test4Output.csv
The model geometry is as specified in Section 2. No DEM is provided as the ground
elevation is uniformly 0.[1]
Technical setup
The setup in this case is a flat surface. It does not require the import of a dem file, since all height values are set to 0.
Other stats:
The grid cell size: 5 m.
The area size: 1010x2010, which includes a border of 5 meters and the required domain of 1000m, x 2000m.
The measurement points have been put on the correct positions, see the image below.
Setup of case 4 used by the Tygron Platform
In order to regulate the water level according to the water level graph, we used the following setup: Only two inlets are used. These are put on the cells above and below the center line indicated by the green line. Each inlet had its own grid cell. The inlets were configured as:
