The raster–vector join reprojects the raster footprint (convex hull of the corners, or envelope) with straight chords and no edge densification, so cross-CRS results can under-/over-cover along curved edges. Densifying the footprint edges (~10 points) before reprojection would improve accuracy for large-extent or very-different-CRS pairs.
This tracks the Sedona (Spark) side. The SedonaDB side: apache/sedona-db#1076.
The raster–vector join reprojects the raster footprint (convex hull of the corners, or envelope) with straight chords and no edge densification, so cross-CRS results can under-/over-cover along curved edges. Densifying the footprint edges (~10 points) before reprojection would improve accuracy for large-extent or very-different-CRS pairs.
This tracks the Sedona (Spark) side. The SedonaDB side: apache/sedona-db#1076.