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Uncertainties associated with digital elevation models for hydrologic applications: a review
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Abstract
Abstract. Digital elevation models (DEMs) represent the topography that drives surface flow and are arguably one of the more important data sources for deriving variables used by numerous hydrologic models. A considerable amount of research has been conducted to address uncertainty associated with error in digital elevation models (DEMs) and the propagation of error to derived terrain parameters. This review brings together a discussion of research in fundamental topical areas related to DEM uncertainty that affect the use of DEMs for hydrologic applications. These areas include: (a) DEM error; (b) topographic parameters frequently derived from DEMs and the associated algorithms used to derive these parameters; (c) the influence of DEM scale as imposed by grid cell resolution; (d) DEM interpolation; and (e) terrain surface modification used to generate hydrologically-viable DEM surfaces. Each of these topical areas contributes to DEM uncertainty and may potentially influence results of distributed parameter hydrologic models that rely on DEMs for the derivation of input parameters. The current state of research on methods developed to quantify DEM uncertainty is reviewed. Based on this review, implications of DEM uncertainty and suggestions for the GIS research and user communities are offered.
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The reduced error distribution for ANADEM could lead to more accurate predictions of hydrological processes, which are particularly sensitive to topographic variations.
“The reduced error distribution shown in Figure 3 for ANADEM could lead to more accurate predictions of hydrological processes, which are particularly sensitive to topographic variations [55,56].”
From ANADEM: A Digital Terrain Model for South America (2024) · cites this paper as [56]
DEM inaccuracies can significantly influence derived information such as watershed delineation, slope, aspect, and drainage network.
“DEM inaccuracies can significantly influence the information derived, such as watershed delineation, slope, aspect, and drainage network [56,58].”
From ANADEM: A Digital Terrain Model for South America (2024) · cites this paper as [56]
The unreliability of DEMs in non-mountainous regions is likely to remain a problem.
“Although efforts have been made to address uncertainty associated with error (e.g. by quantifying DEM accuracy using the Root Mean Square Error (RMSE) statistic (Wechsler 2007: 1483)), the unreliability of DEMs in non-mountainous regions is likely to remain a problem.”
From ‘Benefit Maximizing Routes’: Development and Evaluation Using the Historical Roads of Korea’s Joseon Dynasty (1392–1910) (2022) · cites this paper as Wechsler 2007: 1483
DEMs contain inherent errors, particularly in areas of low slope gradient or areas which lack topographic obstacles.
“As digital representations of topography, DEMs contain inherent errors (i.e. errors in data acquisition subsystems and errors generated during interpolation or aggregation techniques (Wechsler 2007: 1482)), particularly in areas of low slope gradient or areas which lack topographic obstacles.”
From ‘Benefit Maximizing Routes’: Development and Evaluation Using the Historical Roads of Korea’s Joseon Dynasty (1392–1910) (2022) · cites this paper as Wechsler 2007: 1482
The unreliability of both HPMS-based routes and slope gradient-based LCPs in non-mountainous regions stems from problems associated with DEMs, which contain inherent errors particularly in areas of low slope gradient or areas lacking topographic obstacles.
“Firstly, the unreliability of both HPMS-based routes and slope gradient-based LCPs in non-mountainous regions stem from the problems associated with DEMs, which are used to construct cost surfaces. As digital representations of topography, DEMs contain inherent errors (i.e. errors in data acquisition subsystems and errors generated during interpolation or aggregation techniques (Wechsler 2007: 148”
From ‘Benefit Maximizing Routes’: Development and Evaluation Using the Historical Roads of Korea’s Joseon Dynasty (1392–1910) (2022) · cites this paper as Wechsler 2007: 1482
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Validation of surface height from shuttle radar topography mission using shuttle laser altimeter
Sun, G., Ranson, K. J., Kharuk, V. I., & Kovacs, K. (2003) · Remote Sensing of Environment · doi:10.1016/j.rse.2003.09.001 · Cited by 233
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Metadata
- Authors
- Wechsler, S. P.
- Venue
- Hydrology and Earth System Sciences
- Publisher
- Copernicus GmbH
- Published
- 2007-08-03
- Volume
- 11
- Issue
- 4
- Pages
- 1481-1500
- ISSN
- 1607-7938
- Cited by
- 280
- References
- 1
- Language
- en
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
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