Why is the catchment smaller than expected?
Real DEMs contain flats and depressions. D8 flow stops there unless terrain is hydrologically conditioned first. The selected outlet and raster extent also constrain the result.
Free · Local file processing · No account
Compute downslope flow accumulation and the cells draining to a chosen outlet.
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If processing fails, check the file extension and source contents. Use a smaller batch if memory runs low. The original files are never overwritten. Inspect known locations and attributes before sharing a result.
Real DEMs contain flats and depressions. D8 flow stops there unless terrain is hydrologically conditioned first. The selected outlet and raster extent also constrain the result.
Yes. Files and calculations stay in your browser. Page resources require an initial network load. Map previews can request external map tiles. No account is needed.
Use your original elevation DEM for the terrain analyses below. Slope, aspect, visibility and flow grids describe derived values; they are not elevation inputs. Download the raster reference JSON with ASCII outputs to retain their CRS and cell metadata.
Sample terrain along a route and export elevation against distance.
Calculate terrain steepness and downslope direction from an elevation grid.
Summarize valid raster values and inspect the distribution without uploading a GeoTIFF.
Estimate which terrain cells are visible from an observer using a local DEM.