Bare-earth DEM Generation from ArcticDEM, and Its Use in Flood Simulation
- School of Geographical Sciences, University of Bristol, Bristol, UK
- School of Geographical Sciences, University of Bristol, Bristol, UK
Abstract. In urban areas, topography data without above ground objects are typically preferred in wide-area flood simulation, but are not yet available for many locations globally. High-resolution satellite photogrammetry DEMs, like ArcticDEM, are now emerging and could prove extremely useful for global urban flood modelling, however approaches to generate bare-earth DEMs from them have not yet been fully investigated. In this paper, we test the use of two morphological filters (Simple Morphological Filter-SMRF and Progressive Morphological Filter-PMF) to remove surface artefacts from ArcticDEM using the city of Helsinki (192 km2) as a case study. The optimal filter is selected and used to generate a bare-earth version of ArcticDEM. Using a LIDAR DTM as a benchmark, the elevation error and flooding simulation performance for a pluvial event were then evaluated at 2 m and 10 m spatial resolution, respectively. The SMRF was found to be more effective at removing artefacts than PMF over a broad parameter range. For the optimal ArcticDEM-SMRF the elevation RMSE was reduced by up to 70 % over the uncorrected DEM, achieving a final value of 1.02 m. The simulated water depth error was reduced to 0.3 m, which is comparable to typical model errors using LIDAR DTM data. This paper indicates that the SMRF can be directly applied to generate a bare-earth version of ArcticDEM in urban environments, although caution should be exercised for areas with densely packed buildings or vegetation. The results imply that where LIDAR DTMs do not exist, widely available high-resolution satellite photogrammetry DEMs could be used instead.
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Yinxue Liu et al.
Status: closed
-
RC1: 'Comment on nhess-2022-210', Dai Yamazaki, 21 Sep 2022
<General Comments>
The proposed research compared the different surface object removal method on Arctic DEM, and analyzed how DEM error correction impacts flood inundation simulation. Considering increasing availability of high-resolution DEM, I think the suggestions from this research (which correction method is better, which parameters are feasible, how correction impact flood inundation simulation) is very useful. It is good to see that the DEM error correction using SMRF method is robust using wide range of parameters.
One major suggestion I’d like to provide to enhance the manuscript is to include more discussion on the transferability of the proposed method (SMRF algorithm with optimum parameter range) to other regions. Readers must be interested in whether the optimum SMRF parameters detected by this study can be safely used to other regions or not. Please include some discussions about the parameter transferability (detailed suggestions are in the Specific Comments.)Other than the above concern, the manuscript is I think very well organized. And it can be accepted after minor revision.
<Specific Comments>
Line 41: “exponentially increased computational costs”.
“Exponentially” is not precise. The calculation cost of 2D flow simulation follows approximately (1/dx)^3 where dx is the special resolution. If grid size becomes half, the computational cost is almost 8 (=2^3) times, it’s not exponential.
Line 78: ASTER GDEM
Why not including AW3D DEM in reference here, which is more preceise and now being widely used as high-accuracy stereo-view DEM?
L84: SETSM
Please explain what “SETSM” stands for? When it appears first time.
P257: Table 1I suggest to put a line to distinguish PMF and SMRF, as the boundary is not clear.
P270: Replaced with the LIDAR DTM values.
Please describe the situation of the Arctic DEM original value here. Are they “missing data”, or there are large error?
P278: ensuring that the difference between the simulations was distinguishable.
The logic here is unclear. If large-magnitude flood is used as a test case, I assume flood extent is more confined by large-scale topography. Focusing on smaller-magnitude flood might be better to discuss the impact of topography improvement on flood risk estimation.
P286: small isolated wet areas
Please explain the mechanism of how these are caused?
P347: Figure 4
I don’t think the cross marks for man error (right column) are meaningful. The optimum points exist as a “line” in white-color area, rather than as a point in case of the mean error. Putting one cross mark could be miss-leading.
L361: More than 40% of the parameter combinations can 362 reduce the RMSE by greater than a half.
This is important, but there must be something more to discuss for ensuring the robustness of the method. [1] The optimum combinations are almost same for three different land covers, suggesting the robustness of the parameter for various-time land-surface characteristics. [2] The skill-score does not significantly drop when parameter combination is slightly changed from the optimum location, suggesting the robustness of estimated parameters. There must suggest the transferability of the method to another region?
L379: The error distribution of…
Please connect this sentence to the following paragraph. One sentence paragraph is not recommended.
L382: Figure 5
The blue color overlaid on satellite map is very difficult to see. Please adjust colors.
L405: Figure 6:
Can you add one more “cross symbol” which represent the result of the best optimum parameter combination (which are common in all land covers). Readers must be interested in how “best-corrected DEM performs” simultaneously for all skill scores for all land covers.
L446: ArcticDEM-SMRF with larger error.
What do you mean by “error” is not clear here. Do you mean “larger elevation error”?
L450: shown at the spike areas in Fig6
I cannot find where is “the spike” in Figure 6. Please provide better explanation.
L458: Figure 7
Please check the color map of the bottom figure. It seems there are many “green” colors which is not in the color bar.
L517: similarly good flood simulation
I agree that the flood extents are almost similar, but how about flood depth? Can we say “similar”?
L543: ICESAT2
It should be “ICESat-2”.
L589: which resulted in an optimal window size of 30 m and slope threshold of 0.07 in the city of Helsinki.
Please make some discussions on the possibility of transferring this parameter to other regions, or possibility of estimating best parameter for other regions (without Lidar DEM coverage). Readers must be interested in this. If the parameter has relationship to land object characteristic (such as typical building size), there might be a chance to find good parameters for other regions.
-
AC1: 'Reply on RC1', Yinxue Liu, 18 Dec 2022
The comment was uploaded in the form of a supplement: https://nhess.copernicus.org/preprints/nhess-2022-210/nhess-2022-210-AC1-supplement.pdf
-
AC1: 'Reply on RC1', Yinxue Liu, 18 Dec 2022
-
RC2: 'Comment on nhess-2022-210', Guy J.-P. Schumann, 06 Nov 2022
This paper is a comparison of the ArcticDEM vs LiDAR for urban flood simulation which uses Helsinki as an example case.
The paper is generally well written and follows a clear structure. The methodology used is sound and fairly straightforward. The results are well presented.
This type of analysis is quite timely as there are at present substantial efforts and initiatives under way to get better accuracy global DEM data sets and a DEM like the ArcticDEM may become available sson for global low-lying lands.
In my opinion this paper can be accepted for publication after some minor points are addressed:
- Please verify that referring to DigitalGlobe is correct or should it be Maxar?
- It seems to me that the vertical error of the bare earth ArcticDEM in the urban area is about 0.5 m and the simulated water depth RMSE is almost double. If this is correct, could the authors comment on this in the context of whether this type of water depth RMSE in urban areas is still acceptable?
- It would be useful I think if the authors could comment on the resolvability of individual buildings within the ArcticDEM - I imagine some kind of density measure should allow a comparison between LiDAR DSM and ArcticDEM DSM, the results of which could explain the significant differences in water depth RMSE obtained. Maybe some kind of DSM surface roughness measure comparison.
- Could the authors comment on how transferable their presented method and error statistics would be to other urban use cases.
-
AC2: 'Reply on RC2', Yinxue Liu, 18 Dec 2022
The comment was uploaded in the form of a supplement: https://nhess.copernicus.org/preprints/nhess-2022-210/nhess-2022-210-AC2-supplement.pdf
-
AC2: 'Reply on RC2', Yinxue Liu, 18 Dec 2022
Status: closed
-
RC1: 'Comment on nhess-2022-210', Dai Yamazaki, 21 Sep 2022
<General Comments>
The proposed research compared the different surface object removal method on Arctic DEM, and analyzed how DEM error correction impacts flood inundation simulation. Considering increasing availability of high-resolution DEM, I think the suggestions from this research (which correction method is better, which parameters are feasible, how correction impact flood inundation simulation) is very useful. It is good to see that the DEM error correction using SMRF method is robust using wide range of parameters.
One major suggestion I’d like to provide to enhance the manuscript is to include more discussion on the transferability of the proposed method (SMRF algorithm with optimum parameter range) to other regions. Readers must be interested in whether the optimum SMRF parameters detected by this study can be safely used to other regions or not. Please include some discussions about the parameter transferability (detailed suggestions are in the Specific Comments.)Other than the above concern, the manuscript is I think very well organized. And it can be accepted after minor revision.
<Specific Comments>
Line 41: “exponentially increased computational costs”.
“Exponentially” is not precise. The calculation cost of 2D flow simulation follows approximately (1/dx)^3 where dx is the special resolution. If grid size becomes half, the computational cost is almost 8 (=2^3) times, it’s not exponential.
Line 78: ASTER GDEM
Why not including AW3D DEM in reference here, which is more preceise and now being widely used as high-accuracy stereo-view DEM?
L84: SETSM
Please explain what “SETSM” stands for? When it appears first time.
P257: Table 1I suggest to put a line to distinguish PMF and SMRF, as the boundary is not clear.
P270: Replaced with the LIDAR DTM values.
Please describe the situation of the Arctic DEM original value here. Are they “missing data”, or there are large error?
P278: ensuring that the difference between the simulations was distinguishable.
The logic here is unclear. If large-magnitude flood is used as a test case, I assume flood extent is more confined by large-scale topography. Focusing on smaller-magnitude flood might be better to discuss the impact of topography improvement on flood risk estimation.
P286: small isolated wet areas
Please explain the mechanism of how these are caused?
P347: Figure 4
I don’t think the cross marks for man error (right column) are meaningful. The optimum points exist as a “line” in white-color area, rather than as a point in case of the mean error. Putting one cross mark could be miss-leading.
L361: More than 40% of the parameter combinations can 362 reduce the RMSE by greater than a half.
This is important, but there must be something more to discuss for ensuring the robustness of the method. [1] The optimum combinations are almost same for three different land covers, suggesting the robustness of the parameter for various-time land-surface characteristics. [2] The skill-score does not significantly drop when parameter combination is slightly changed from the optimum location, suggesting the robustness of estimated parameters. There must suggest the transferability of the method to another region?
L379: The error distribution of…
Please connect this sentence to the following paragraph. One sentence paragraph is not recommended.
L382: Figure 5
The blue color overlaid on satellite map is very difficult to see. Please adjust colors.
L405: Figure 6:
Can you add one more “cross symbol” which represent the result of the best optimum parameter combination (which are common in all land covers). Readers must be interested in how “best-corrected DEM performs” simultaneously for all skill scores for all land covers.
L446: ArcticDEM-SMRF with larger error.
What do you mean by “error” is not clear here. Do you mean “larger elevation error”?
L450: shown at the spike areas in Fig6
I cannot find where is “the spike” in Figure 6. Please provide better explanation.
L458: Figure 7
Please check the color map of the bottom figure. It seems there are many “green” colors which is not in the color bar.
L517: similarly good flood simulation
I agree that the flood extents are almost similar, but how about flood depth? Can we say “similar”?
L543: ICESAT2
It should be “ICESat-2”.
L589: which resulted in an optimal window size of 30 m and slope threshold of 0.07 in the city of Helsinki.
Please make some discussions on the possibility of transferring this parameter to other regions, or possibility of estimating best parameter for other regions (without Lidar DEM coverage). Readers must be interested in this. If the parameter has relationship to land object characteristic (such as typical building size), there might be a chance to find good parameters for other regions.
-
AC1: 'Reply on RC1', Yinxue Liu, 18 Dec 2022
The comment was uploaded in the form of a supplement: https://nhess.copernicus.org/preprints/nhess-2022-210/nhess-2022-210-AC1-supplement.pdf
-
AC1: 'Reply on RC1', Yinxue Liu, 18 Dec 2022
-
RC2: 'Comment on nhess-2022-210', Guy J.-P. Schumann, 06 Nov 2022
This paper is a comparison of the ArcticDEM vs LiDAR for urban flood simulation which uses Helsinki as an example case.
The paper is generally well written and follows a clear structure. The methodology used is sound and fairly straightforward. The results are well presented.
This type of analysis is quite timely as there are at present substantial efforts and initiatives under way to get better accuracy global DEM data sets and a DEM like the ArcticDEM may become available sson for global low-lying lands.
In my opinion this paper can be accepted for publication after some minor points are addressed:
- Please verify that referring to DigitalGlobe is correct or should it be Maxar?
- It seems to me that the vertical error of the bare earth ArcticDEM in the urban area is about 0.5 m and the simulated water depth RMSE is almost double. If this is correct, could the authors comment on this in the context of whether this type of water depth RMSE in urban areas is still acceptable?
- It would be useful I think if the authors could comment on the resolvability of individual buildings within the ArcticDEM - I imagine some kind of density measure should allow a comparison between LiDAR DSM and ArcticDEM DSM, the results of which could explain the significant differences in water depth RMSE obtained. Maybe some kind of DSM surface roughness measure comparison.
- Could the authors comment on how transferable their presented method and error statistics would be to other urban use cases.
-
AC2: 'Reply on RC2', Yinxue Liu, 18 Dec 2022
The comment was uploaded in the form of a supplement: https://nhess.copernicus.org/preprints/nhess-2022-210/nhess-2022-210-AC2-supplement.pdf
-
AC2: 'Reply on RC2', Yinxue Liu, 18 Dec 2022
Yinxue Liu et al.
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