ORMGP Topological Watercourses
Description
The Ontario Hydro Network (OHN) - Watercourse layer offered by the Ontario Ministry of Natural Resources and Forestry has been analyzed based on a spatial analysis to define a connectivity network and a directional graph. Watercourse channel segments are topologically correct, meaning that every segments is defined by its upstream and downstream segments.
- Type
- Vector - Polyline shapefile.
- Geographic Extent
- The extended ORMGP Study Area covering the Niagara peninsula to the Bay of Quinty.
- Maintenance Standard
- Periodically updated in coordination with OHN updates.
Georeferencing and Accuracy
- Horizontal Datum
- North American Datum 1983
- 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) Sub-Watersheds.
- Agency Originator
- Oak Ridges Moraine Groundwater Program (ORMGP)
- Agency Distributor
- Oak Ridges Moraine Groundwater Program (ORMGP)
Methodology
- Data Source - Ontario Hydro Network (OHN) - Watercourse
- See Source metadata
- Vector Processing
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OHN watercourse layer is reprojected to EPGS 3161
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Watercourses are “segmentized”: polylines are defined as single linear features from junction to junction.
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Certain stream segments were manually removed in order to prevent “unnatural” flow connectivity. (This commonly occurs along man-made canal routes such as the Trent-Severn waterway.)
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An adjacency matrix is built to collect segment endpoints that are close to one another. Adjacency is assumed to imply segment connectivity.
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topological ordering is then performed, attributing segments with their appropriate Strahler (1952) code.
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- Replaces or Updates
- Oak Ridges Moraine Groundwater Program (v2020) sub-watershed layer.
- References
- Strahler, A.N., 1952. Hypsometric (area-altitude) analysis of erosional topology, Geological Society of America Bulletin 63(11): 1117–1142.
- Contact
- email (support@owrc.ca)
Last Modified: 2024-03-24