Hydrologically Conditioned Digital Elevation Model (HDEM)
Description
The Provincial Digital Elevation Model (PDEM) offered by the Ontario Ministry of Natural Resources and Forestry has been up-scaled and conditioned to acquire continuous flow paths. This product is necessary for catchment delineation to any point within the extended ORMGP boundary.
- Type
- Raster - Gridded on 60m cells.
- Geographic Extent
- The extended ORMGP Study Area covering the Niagara peninsula to the Bay of Quinty.
- Maintenance Standard
- Periodically updated in coordination with PDEM updates and by noted flowpath discrepancies discovered by our user base (see Manual Adjustments below).
Georeferencing and Accuracy
- Horizontal Datum
- North American Datum 1983
- Vertical Datum
- CGVD2013 (EPSG 6647)
- Ellipsoid
- GRS 1980
- Prime meridian
- Greenwich
- Projection
- Ontario MNR Lambert (EPSG 3161)
- Horizontal Accuracy
- 1.5m
- Unit
- metre
- Information source
- Ontario Ministry of Natural Resources via Conservation Ontario.
Data Sources and Restrictions
- Use Constraint
- None - in accordance with ORMGP disclaimer
- Citation
- Oak Ridges Moraine Ground Water Program (2023) Hydro-DEM.
- Agency Originator
- Oak Ridges Moraine Groundwater Program (ORMGP)
- Agency Distributor
- Oak Ridges Moraine Groundwater Program (ORMGP)
Methodology
- Data Source - Provincial Digital Elevation Model (PDEM)
- See source metadata.
- Raster Upscaling
- PDEM is upscaled from a 30m horizontal resolution to 60m by taking the mean of the 4 intersecting cells.
- Raster Processing
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Automated depression filling (Wang and Liu, 2006) was applied to the DEM.
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Flat regions were adjusted according to the depression filling fix of Garbrecht and Martz (1997).
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Flow paths are computed based on the “D8” algorithm (O’Callaghan and Mark, 1984).
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Manual Adjustments
- Flow directions are imposed using hand-drawn flow paths where the algorithm fails to discover the true flow direction. Flow paths are save as polyline shapefiles, where its vertices are ordered according to flow direction.
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Derivative Products
- Cell slopes and slope-aspects are computed using a 9-point planar regression from every cell’s elevation plus its 8 neighbouring grid elevations.
- Replaces or Updates
- Oak Ridges Moraine Groundwater Program (v2020) HDEM.
- References
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Garbrecht, J, and L. Martz, 1997. The assignment of drainage direction over flat surfaces in raster digital elevation models. Journal of Hydrology, 193, 204-213.
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O’Callaghan, J.F., and D.M. Mark, 1984. The extraction of drainage net-works from digital elevation data, Comput. Vision Graphics Image Process., 28, pp. 328-344
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Wang, L., H. Liu, 2006. An efficient method for identifying and filling surface depressions in digital elevation models for hydrologic analysis and modelling. International Journal of Geographical Information Science 20(2): 193-213.
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- Contact
- email (support@owrc.ca)
Last Modified: 2024-03-24