Entry
025
Source scale
0.5 m grid
Method
Airborne laser, classified returns
Section
Canopy
An oblique aerial view of a worked site beside water

A half-metre grid records more than a sheet can show, and the drawing spacing still has to be chosen afterwards.

Photo: Ferdie Cayanga / Pexels

What fits in fifty centimetres

When a lidar-derived terrain model is gridded at half-metre resolution, each cell represents a ground patch roughly the size of a paving slab. At that scale, individual plough ridges — typically 30 to 60 centimetres from crest to trough — become legible as distinct rows of alternating high and low returns. Ridge-and-furrow earthworks that vanish completely at the two-metre resolution common in national archive products reappear as unmistakable corrugation. The difference is not cosmetic; it changes what can be measured and what can be missed.

National mapping agencies that operate at this resolution tend to acquire their data at point densities of four returns per square metre or higher — the minimum needed to produce a reliable half-metre bare-earth surface under vegetation. Below that density, the grid interpolates rather than records, and the interpolation can smear exactly the kind of sharp edge a furrow provides.

A false-colour elevation surface with contour lines threaded through it

A surface has to be cut at some spacing before it can be drawn, and the spacing is chosen rather than measured.

Photo: kdadan97 / Pexels

The storage consequence is direct and not trivial. A half-metre grid covers four times the cells of a one-metre grid over the same area, and sixteen times those of a two-metre grid. A single one-kilometre tile in 32-bit floating-point raster format runs to around sixteen megabytes. A national coverage at that resolution — across a country the size of England — sits in the low terabytes, manageable by modern infrastructure but not negligible when every derivative product (slope, aspect, hillshade, curvature) requires its own layer at the same grain.

Tiling conventions matter here more than they do at coarser resolutions. A query that crosses a tile boundary must stitch two or more files, and if the tiles were not classified consistently, a seam can run across a field as a thin discontinuity in elevation values — invisible on a hillshade but measurable in a profile.

A survey instrument on a desk beside a window, a map and drawing tools laid out

Field and desk are separate operations, reconciled only where control has been established.

For anyone using half-metre data seriously, the practical question is not whether the resolution is high enough. It almost always is. The question is whether the acquisition density, the classification parameters, and the tiling scheme were applied consistently enough for the detail the grid appears to offer to be real.

What the numbers mean4 figures
0.5 m resolutionfour cells per square metre of ground; each cell is roughly paperback-book sized
4 returns per m²typical minimum point density for a reliable half-metre bare-earth surface
~4 MBapproximate size of a single 1 km tile in 32-bit floating-point format
16×the cell-count increase moving from a 2 m grid to a 0.5 m grid over the same area

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Canopy