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The river estimation approach appears to introduce an 'wall artefact' down river amplified from any high elevation values detected along the measured cross section data.
As an example:
"See below the strange artifact of a ridgeline in the river that seems like an exaggerated version of a small positive feature in the surveyed XS (0.5 m), increased to 3 m in the interpolated data and extending to the next XS upstream and downstream."
The river estimation approach appears to introduce an 'wall artefact' down river amplified from any high elevation values detected along the measured cross section data.
As an example:
"See below the strange artifact of a ridgeline in the river that seems like an exaggerated version of a small positive feature in the surveyed XS (0.5 m), increased to 3 m in the interpolated data and extending to the next XS upstream and downstream."
Starting point:
Could it be due to the taking the nearest point along the measured sections instead of interpolating the value nearest to the sample locations.. https://github.com/rosepearson/GeoFabrics/blob/main/src/geofabrics/bathymetry_estimation.py#L772
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