Stream Extraction

Extract a stream network by thresholding flow accumulation, optionally expressing the threshold as contributing-cell count or drainage area.

HydrologyEnd-User DocumentationTheory + Formula + Parameters

1. What This Feature Does

Extract a stream network by thresholding flow accumulation, optionally expressing the threshold as contributing-cell count or drainage area.

Cloud workflow: choose data → configure the scientific method → run → review the resulting layer/report. No programming is required.

2. Recommended Workflow

Choose DEM/elevation band. ↓ Optionally fill sinks. ↓ Compute flow direction and accumulation. ↓ Choose threshold unit and value. ↓ Create the stream raster/network. ↓ Calibrate the threshold against known hydrography or imagery.

3. Theory, Methods & Equations

Contributing-Cell Threshold

A cell becomes stream when upstream cell accumulation exceeds a threshold.

Stream(p)=1 if A(p) ≥ Tcells
Best used when: working directly in raster-cell units.

Drainage-Area Threshold

Converts accumulation to contributing area using pixel area.

Area(p)=A(p)×Acell
Stream(p)=1 if Area(p) ≥ Tarea
Best used when: a physically interpretable catchment-area threshold is preferred.

4. Input Data

InputTypeRequirementDescription
DEM RasterrasterRequired

5. Parameters Available in the Application

ParameterDefaultChoices / RangeHow to Use It
Elevation Band
Fill Sinks FirstOn
Threshold UnitcellsContributing Cells, Drainage Area (km²)
Stream Threshold10000.0001 to —

6. Output & Interpretation

The result should be interpreted according to the selected method and the physical meaning of the input data. Preserve source units, coordinate reference information, NoData meaning, acquisition date, and preprocessing level when comparing results.

Scientific interpretation: an algorithm can produce a numerically valid result even when the input data are unsuitable. Always check masks, units, sensor characteristics, spatial resolution and reference data.

7. Best Practices

  • Use analysis-ready inputs and remove invalid/cloud/noise artifacts that are not part of the target phenomenon.
  • Choose parameters from the physical scale of the data, not only from visual appearance.
  • Keep categorical and continuous rasters conceptually separate when selecting interpolation/resampling methods.
  • Compare the result with the source image and independent reference information.
  • Document the settings used when results will be compared across dates, sensors or study areas.