UK EA benchmark 2 (Water Module): Difference between revisions
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[[Image:result_case2_ukbm.gif|right|Animation of the test result for case 2, generated by the {{software}}. Map dimensions = 2,000 x 2,000 m. Grid-cell size = 5 m.]] | |||
This [[Water Module benchmarks|benchmark]] performs test case 2 of the UK EA benchmark named '''Test 2 – Filling of Floodplain Depressions''', using the {{software}}.__NOTOC__ | |||
The test has been designed to evaluate the capability of a package to determine inundation extent and final flood depth, in a case involving low momentum flow over a complex topography.<ref name="Néelz"/> | |||
A copy of this test project is made available to everyone, providing hands-on insights to those interested. The project can be found on the LTS server under the name '''UKEA benchmark 2'''. This is covered in more detail in [[UK EA benchmark 2 (Water Module)#Public test project|this]] section. | |||
<br style="clear:both"> | <br style="clear:both"> | ||
==Description== | ==Description== | ||
[[File:dem_case2_ukbm.png| | [[File:dem_case2_ukbm.png|left|thumb|400px|Fig. (a): Map of the DEM showing the location of the upstream boundary condition (red line), ground elevation contour lines every 0.05 m and output point locations (crosses).]] | ||
The area modelled, shown in Fig. (a), is a perfect 2,000 m x 2,000 m square and consists of a 4 x 4 matrix of ~0.5-m deep depressions with smooth topographic transitions. The DEM (digital elevation model) was obtained by multiplying sinusoids in the north to south and west to east directions, and the resulting depressions are all identical in shape. An underlying average slope of 1:1,500 exists in the north to south direction, and of 1:3,000 in the west to east direction, with a ~2-m drop in elevation along the north-west to south-east diagonal.<ref name="Néelz"/> | |||
The inflow boundary condition was applied along a 100-m line running south from the northwestern corner of the modelled domain, indicated by a red line in Fig. (a). A flooding with a peak flow of 20 m<sup>3</sup>/s and time base of ~85 minutes was implemented according the hydrograph in Fig. (b). The model was run for 2 days (48 hours) to allow the inundation to settle to its final state.<ref name="Néelz"/> | |||
[[File:flood_hydrograph_case2_ukbm.png|left|thumb|x200px|Fig. (b): Inflow hydrograph, which functioned as upstream boundary condition]] | [[File:flood_hydrograph_case2_ukbm.png|left|thumb|x200px|Fig. (b): Inflow hydrograph, which functioned as upstream boundary condition]] | ||
Line 17: | Line 18: | ||
==Initial and boundary conditions== | ==Initial and boundary conditions== | ||
*Initial condition: dry bed | * Initial condition: dry bed | ||
*Inflow along the red line in Fig. (a) | * Inflow along the red line in Fig. (a) | ||
*All other boundaries are closed | * All other boundaries are closed | ||
==Parameter values== | ==Parameter values== | ||
*Manning’s ''n'': 0.03 (uniform) | * Manning’s ''n'': 0.03 (uniform) | ||
*Model grid resolution: 20 m ( | * Model grid resolution (m): 20 m (or ~10,000 nodes in the area modelled) | ||
*Simulated time: 48 | * Simulated time (h): 48 | ||
==Technical setup== | ==Technical setup== | ||
Line 30: | Line 31: | ||
<ul> | <ul> | ||
<li style="display:inline-block">[[File:hmapori_case2_ukbm.png|thumb|x353px|Original 2-m heightmap (2,400 m x 2,400 m)]]</li> | <li style="display:inline-block">[[File:hmapori_case2_ukbm.png|thumb|x353px|Original 2-m heightmap (2,400 m x 2,400 m)]]</li> | ||
<li style="display:inline-block">[[File:hmapcrop_case2_ukbm.png|thumb|x300px|Cropped and rescaled to 20-m grid ( | <li style="display:inline-block">[[File:hmapcrop_case2_ukbm.png|thumb|x300px|Cropped and rescaled to 20-m grid (2,040 m x 2,040 m). The black perimeter designates the border cells.]]</li> | ||
<li style="display:inline-block">[[File:inlets_case2_ukbm.png|thumb|x300px|Inlet series in the upper left corner.]]</li> | <li style="display:inline-block">[[File:inlets_case2_ukbm.png|thumb|x300px|Inlet series in the upper left corner.]]</li> | ||
</ul> | </ul> | ||
Line 36: | Line 37: | ||
In order to regulate the water level according to the water-level graph, the following setup was used: | In order to regulate the water level according to the water-level graph, the following setup was used: | ||
Inlet objects were placed on single grid cells with a constant value for ''x'' = 1 and ''y'' varying from 1 to 5, yielding a total of 5 points. The inlets were configured as follows: | Inlet objects were placed on single grid cells with a constant value for ''x'' = 1 and ''y'' varying from 1 to 5, yielding a total of 5 points. The inlets were configured as follows: | ||
* External area ( | * External area (m<sup>2</sup>): 1,000,000,000 (default) | ||
* Water level (m): 1 | * Water level (m): 1 (default) | ||
* Threshold (m): none | * Threshold (m): none (default) | ||
* Inlet Q (m<sup>3</sup>/s) : 20 in total, thus 4 per inlet | * Inlet Q (m<sup>3</sup>/s) : 20 in total, thus 4 per inlet | ||
[[File:inlet_q_case2_ukbm.png|thumb|x300px|left|Hydrograph for each individual inlet.]] | [[File:inlet_q_case2_ukbm.png|thumb|x300px|left|Hydrograph for each individual inlet.]] | ||
Line 45: | Line 46: | ||
==Output as required== | ==Output as required== | ||
===Stats=== | ===Stats=== | ||
*Software package used: {{software}} | * Software package used: {{software}} | ||
*Numerical scheme: FV (Kurganov, Bollerman, Horvath) | * Numerical scheme: [[Surface flow formula (Water Overlay)|FV (Kurganov, Bollerman, Horvath)]] | ||
* Object flow (m<sup>3</sup>/s): 96,985.64 | |||
* Remaining volume water (m<sup>3</sup>/s): 96,982.30 | |||
*Object flow | |||
*Remaining volume water | |||
===Test results=== | ===Test results=== | ||
Line 131: | Line 124: | ||
</ul> | </ul> | ||
==Notes== | ===Notes=== | ||
* Tests were run with a multi-GPU setup. For small cases like this, using single GPU actually leads to faster results. Furthermore, requesting a high number of 576 timeframes further bogs it down. In comparison: 1 GPU with 1 resulting timeframe runs in: 8 s, which is +- 53% faster compared to 2 GPUs with 576 timeframes. | * Tests were run with a multi-GPU setup. For small cases like this, using single GPU actually leads to faster results. Furthermore, requesting a high number of 576 timeframes further bogs it down. In comparison: 1 GPU with 1 resulting timeframe runs in: 8 s, which is +- 53% faster compared to 2 GPUs with 576 timeframes. | ||
==Public test project== | |||
A copy of this test project is made available to everyone | A copy of this test project is made available to everyone, providing hands-on insights to those interested. The project can be found on the LTS server under the name '''UKEA benchmark 2'''. In this project the discussed benchmark test is reproduced, based on a map size of 2,040 m x 2,040 m to compensate for the 20-m border cells. These special map dimensions are generally not selectable in the [[New Project Wizard]] and require configuration through the [[API]]. | ||
===Measurement points=== | |||
The locations of the measurement points are: | |||
{|class="wikitable" style="display: inline-table;" | {|class="wikitable" style="display: inline-table;" | ||
!Point ID | !Point ID | ||
Line 145: | Line 139: | ||
|1 | |1 | ||
|275 | |275 | ||
| -1, | | -1,780 | ||
|- | |- | ||
|2 | |2 | ||
|275 | |275 | ||
| -1, | | -1,290 | ||
|- | |- | ||
|3 | |3 | ||
|275 | |275 | ||
| - | | -790 | ||
|- | |- | ||
|4 | |4 | ||
|275 | |275 | ||
| - | | -290 | ||
|- | |- | ||
|5 | |5 | ||
| | |775 | ||
| -1, | | -1,780 | ||
|- | |- | ||
|6 | |6 | ||
| | |775 | ||
| -1, | | -1,290 | ||
|- | |- | ||
|7 | |7 | ||
| | |775 | ||
| - | | -790 | ||
|- | |- | ||
|8 | |8 | ||
| | |775 | ||
| - | | -290 | ||
|} | |} | ||
Line 182: | Line 176: | ||
|- | |- | ||
| 9 | | 9 | ||
| 1, | | 1,275 | ||
| -1, | | -1,780 | ||
|- | |- | ||
| 10 | | 10 | ||
| 1, | | 1,275 | ||
| -1, | | -1,290 | ||
|- | |- | ||
| 11 | | 11 | ||
| 1,255 | | 1,255 | ||
| - | | -790 | ||
|- | |- | ||
| 12 | | 12 | ||
| 1, | | 1,275 | ||
| - | | -290 | ||
|- | |- | ||
| 13 | | 13 | ||
| 1, | | 1,775 | ||
| -1, | | -1,780 | ||
|- | |- | ||
| 14 | | 14 | ||
| 1, | | 1,775 | ||
| -1, | | -1,290 | ||
|- | |- | ||
| 15 | | 15 | ||
| 1, | | 1,775 | ||
| - | | -790 | ||
|- | |- | ||
| 16 | | 16 | ||
| 1, | | 1,775 | ||
| - | | -290 | ||
|} | |} | ||
Note that the coordinate system in this project differs from the one used during the actual benchmark testing as shown in Fig. (b). For the above listed points the center (0,0) is located at the top-left corner instead of the bottom-left, hence will the bottom-right corner have coordinates (2,000;-2,000). | Note that the coordinate system in this project differs from the one used during the actual benchmark testing as shown in Fig. (b). For the above listed points the center (0,0) is located at the top-left corner instead of the bottom-left, hence will the bottom-right corner have coordinates (2,000;-2,000). | ||
===Water level relative to datum=== | |||
The time series of a fixed measurement point can be obtained as follows: | |||
{{Editor steps|title=obtain water levels relative to datum|Go to the flooding overlay "Water Level (m)".|Select the measuring tool.|From the ''Saved'' dropdown choose your point of interest.|From the ''Base'' dropdown select "Surface Elevation (m)".|Make sure the ''Sum'' box is checked.|Select ''Fit Graph'' to zoom in on the relevant part of the plot.}} | |||
===Settings & output=== | |||
{|class="wikitable" style="display: inline-table;" | |||
!Setting | |||
!Unit | |||
!Value | |||
|- | |||
|GRAVITY | |||
|m/s<sup>2</sup> | |||
|9.80665 | |||
|- | |||
|QUAD_CELL | |||
|''Boolean'' | |||
|0 | |||
|- | |||
|WALL_ANGLE | |||
|° | |||
|89 | |||
|- | |||
|Open land | |||
|m<sup>2</sup> | |||
|14,786,560 | |||
|- | |||
|Manning's ''n'' | |||
|s/(m<sup>1/3</sup>) | |||
|0.03 | |||
|- | |||
|Calc. pref. | |||
| | |||
|Accuracy | |||
|} | |||
{|class="wikitable" style="display: inline-table;" | |||
!Output | |||
!Unit | |||
!Value | |||
|- | |||
|Total volume | |||
|m<sup>3</sup> | |||
|97,194 | |||
|- | |||
|Single cells | |||
| | |||
|10,404 | |||
|- | |||
|Calc. steps | |||
| | |||
|250,709 | |||
|- | |||
|Calc. time | |||
|s | |||
|25 | |||
|} | |||
Note that these output values may deviate slightly from those of the initial testing phase (i.e. not the public test project), since there is a substantial time gap between when the two projects were set up, during which several changes have been made to the engine. | |||
==References== | ==References== | ||
<references> | <references> | ||
<ref name="Néelz">Néelz, S., & Pender, G. (2013). Benchmarking the latest generation of 2D hydraulic modelling packages. Report: SC120002. Environment Agency, Horison House, Deanery Road, Bristol, BS1 9AH. ISBN: 978-1-84911-306-9. Retrieved from: https://www.gov.uk/government/publications/benchmarking-the-latest-generation-of-2d-hydraulic-flood-modelling-packages </ref> | |||
<ref name="Néelz">Néelz S., Pender G. (2013) | |||
</references> | </references> | ||
[[Category:Benchmarks]] | [[Category:Benchmarks]] | ||
{{Water Module buttons}} |
Latest revision as of 15:09, 5 March 2024
This benchmark performs test case 2 of the UK EA benchmark named Test 2 – Filling of Floodplain Depressions, using the Tygron Platform.
The test has been designed to evaluate the capability of a package to determine inundation extent and final flood depth, in a case involving low momentum flow over a complex topography.[1]
A copy of this test project is made available to everyone, providing hands-on insights to those interested. The project can be found on the LTS server under the name UKEA benchmark 2. This is covered in more detail in this section.
Description
The area modelled, shown in Fig. (a), is a perfect 2,000 m x 2,000 m square and consists of a 4 x 4 matrix of ~0.5-m deep depressions with smooth topographic transitions. The DEM (digital elevation model) was obtained by multiplying sinusoids in the north to south and west to east directions, and the resulting depressions are all identical in shape. An underlying average slope of 1:1,500 exists in the north to south direction, and of 1:3,000 in the west to east direction, with a ~2-m drop in elevation along the north-west to south-east diagonal.[1]
The inflow boundary condition was applied along a 100-m line running south from the northwestern corner of the modelled domain, indicated by a red line in Fig. (a). A flooding with a peak flow of 20 m3/s and time base of ~85 minutes was implemented according the hydrograph in Fig. (b). The model was run for 2 days (48 hours) to allow the inundation to settle to its final state.[1]
Initial and boundary conditions
- Initial condition: dry bed
- Inflow along the red line in Fig. (a)
- All other boundaries are closed
Parameter values
- Manning’s n: 0.03 (uniform)
- Model grid resolution (m): 20 m (or ~10,000 nodes in the area modelled)
- Simulated time (h): 48
Technical setup
The required DEM is provided as an ASCII file (test2DEM.asc). As its cell size is 2 m, whereas the test is expected to be run on a 20-m grid, it will be automatically rescaled by the grid rasterizer. The dimensions of the test area must be 2,000 by 2,000 m. The original DEM had an offset of -200 m, which was cropped down to -20 m (= 1 grid cell) so it could function as border cell. The rescaled and cropped ASCII file will shortly be provided as part of a .zip found at the bottom of this page.
In order to regulate the water level according to the water-level graph, the following setup was used: Inlet objects were placed on single grid cells with a constant value for x = 1 and y varying from 1 to 5, yielding a total of 5 points. The inlets were configured as follows:
- External area (m2): 1,000,000,000 (default)
- Water level (m): 1 (default)
- Threshold (m): none (default)
- Inlet Q (m3/s) : 20 in total, thus 4 per inlet
Output as required
Stats
- Software package used: Tygron Platform
- Numerical scheme: FV (Kurganov, Bollerman, Horvath)
- Object flow (m3/s): 96,985.64
- Remaining volume water (m3/s): 96,982.30
Test results
Point graph measurements from the Tygron Platform (left) and other packages (right):
Last frame
- Final timeframe of water levels as generated by the Tygron Platform (left) and by the other packages (right).
Notes
- Tests were run with a multi-GPU setup. For small cases like this, using single GPU actually leads to faster results. Furthermore, requesting a high number of 576 timeframes further bogs it down. In comparison: 1 GPU with 1 resulting timeframe runs in: 8 s, which is +- 53% faster compared to 2 GPUs with 576 timeframes.
Public test project
A copy of this test project is made available to everyone, providing hands-on insights to those interested. The project can be found on the LTS server under the name UKEA benchmark 2. In this project the discussed benchmark test is reproduced, based on a map size of 2,040 m x 2,040 m to compensate for the 20-m border cells. These special map dimensions are generally not selectable in the New Project Wizard and require configuration through the API.
Measurement points
The locations of the measurement points are:
Point ID | X | Y |
---|---|---|
1 | 275 | -1,780 |
2 | 275 | -1,290 |
3 | 275 | -790 |
4 | 275 | -290 |
5 | 775 | -1,780 |
6 | 775 | -1,290 |
7 | 775 | -790 |
8 | 775 | -290 |
Point ID | X | Y |
---|---|---|
9 | 1,275 | -1,780 |
10 | 1,275 | -1,290 |
11 | 1,255 | -790 |
12 | 1,275 | -290 |
13 | 1,775 | -1,780 |
14 | 1,775 | -1,290 |
15 | 1,775 | -790 |
16 | 1,775 | -290 |
Note that the coordinate system in this project differs from the one used during the actual benchmark testing as shown in Fig. (b). For the above listed points the center (0,0) is located at the top-left corner instead of the bottom-left, hence will the bottom-right corner have coordinates (2,000;-2,000).
Water level relative to datum
The time series of a fixed measurement point can be obtained as follows:
- Go to the flooding overlay "Water Level (m)".
- Select the measuring tool.
- From the Saved dropdown choose your point of interest.
- From the Base dropdown select "Surface Elevation (m)".
- Make sure the Sum box is checked.
- Select Fit Graph to zoom in on the relevant part of the plot.
Settings & output
Setting | Unit | Value |
---|---|---|
GRAVITY | m/s2 | 9.80665 |
QUAD_CELL | Boolean | 0 |
WALL_ANGLE | ° | 89 |
Open land | m2 | 14,786,560 |
Manning's n | s/(m1/3) | 0.03 |
Calc. pref. | Accuracy |
Output | Unit | Value |
---|---|---|
Total volume | m3 | 97,194 |
Single cells | 10,404 | |
Calc. steps | 250,709 | |
Calc. time | s | 25 |
Note that these output values may deviate slightly from those of the initial testing phase (i.e. not the public test project), since there is a substantial time gap between when the two projects were set up, during which several changes have been made to the engine.
References
- ↑ 1.0 1.1 1.2 Néelz, S., & Pender, G. (2013). Benchmarking the latest generation of 2D hydraulic modelling packages. Report: SC120002. Environment Agency, Horison House, Deanery Road, Bristol, BS1 9AH. ISBN: 978-1-84911-306-9. Retrieved from: https://www.gov.uk/government/publications/benchmarking-the-latest-generation-of-2d-hydraulic-flood-modelling-packages