Forestry

Riparian species and cold seeps on the Scott River

Fourteen riparian species classified across 423 acres of river corridor, with thermal mapping that pointed to groundwater fed cold seeps.

Draft for review. Facts and permission still being confirmed, not indexed, not listed.
Client
Restoration project manager, with a botanist leading field identification
Location
Scott River near Etna, California, Klamath Basin
Years
2025
Lane
Forestry

The problem

Restoration partners needed to know what was growing along the river and where the water stayed cool in summer, the two things that decide fish habitat, at a scale a field crew cannot walk.

What we flew

  • MicaSense RedEdge MX multispectral at 399 feet, 8 cm ground resolution
  • DJI H20T thermal at 399 feet, 10.5 cm ground resolution, morning and afternoon on separate days
  • DJI P1 RGB at 328 feet, 2.2 cm, for review and outreach
  • Georeferenced to crewed aircraft LiDAR, about 1.5 feet horizontal

What we delivered

  • Canopy polygons with tiered species, the most likely species first, for 14 classes
  • Multispectral, NDWI, thermal, and RGB orthomosaics as GeoTIFF
  • Relative elevation model with one foot contours from the LiDAR
  • 20 foot thermal temperature grid and potential cold seep points
  • Classified water, river centerline, and the field sample lines used to train the model
  • An ArcGIS Experience Builder viewer the botanist used to review and correct species calls
  • Written report with method, accuracy, limits, and recommendations

Fourteen species is a hard problem for a classifier. Willows overlap spectrally, canopies overlap physically, and some species had only a handful of samples. The tiered output handles that: every polygon carries its first, second, and third most likely species, and the report says which classes were weak and why.

The thermal work is read as relative temperature. An ice water calibration was attempted, the flight altitude still introduced swings, so the products highlight cooler and warmer zones rather than claiming a surface temperature to the degree. That is enough to find a seep. It is not a surface temperature to the degree, and we do not sell it as one.

Canopy polygons by dominant species with the fourteen class legend.
Canopy polygons by dominant species.
Afternoon thermal mosaic, the river channel dark and cool against warm ground.
Afternoon thermal mosaic. The cooler zones in the channel are the candidates for groundwater inflow.
Relative elevation model with one foot contours across the floodplain.
Relative elevation model with one foot contours, the micro topography that moves water and seeds.
Multispectral mosaic of the reach with crowns outlined.
Multispectral mosaic of the reach.
Thermal orthomosaic of a river reach: the channel reads dark and cool, gravel bars and open ground glow orange and yellow.
One section of the relative temperature raster, rendered straight from the data. Water reads dark and cool, gravel bars warm.
Relative elevation model of a river reach: the channel in dark ink, floodplain surfaces stepping up through grey to the valley floor.
The relative elevation model as a raster, height above the channel from zero to twenty feet.

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