The dimensionless product of drainage density (stream length per unit area – km/km2) and total elevation relief.
— Melton, 1957
The difference between the highest and lowest points in the watershed, relative to watershed length (in km).
— Schumm, 1956
The potential for rapid runoff delivery to and through streams, which may contribute to harmful flood events
— Patton and Baker, 1976
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Generate relief for BC FWA Assessment Watersheds by overlaying with the BC 1:20k DEM
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Calculate drainage density per watershed polygon (km of streams / km2 of watershed) using this definition of 'stream':
- FWA river polygon centerlines
- FWA primary/secondary flow lines (ie,
edge_type IN (1000,1100,2000,2300)and not within a lake/reservoir/wetland waterbody)
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Calculate DDR as drainage density * relief
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Classify DDR:
- class 1: less than 2000 km/km2
- class 2: 2000-4000 km/km2
- class 3: greater than 4000 km/km2
- BC FWA loaded to postgres database defined by
$DATABASE_URLviafwapg jq,parallel- BC DEM
./ddr.sh
ddr.csv
| column | description |
|---|---|
watershed_feature_id |
Assessment watershed unique id |
elevation_min |
Minimum elevation in the watershed (m) |
elevation_max |
Maximum elevation in the watershed (m) |
elevation_relief |
The elevation relief in the watershed (m) |
stream_length_km |
Length of stream in the watershed (km) |
watershed_area_km2 |
Area of the watershed (km2) |
drainage_density |
Total length of streams / total area of watershed (km/km2) |
drainage_density_ruggedness |
Stream density as a function of relief (km of streams / km2 of watershed) * relief |
drainage_dens_rugged_cls_num |
Numeric classification of DDR: (1: <2000; 2: 2000-4000; 3: >= 4000) |