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Geospatial

Global Digital Elevation Model

A seamless, void-filled global digital elevation model — 30 m everywhere, 10 m across many regions, and 1 m across most developed countries.

What this dataset is

A seamless, void-filled global digital elevation model. Resolution is 30 m everywhere as a floor, sharpening to 10 m across many regions where higher-quality public radar or stereo-photogrammetry is available, and to 1 m across most developed countries where national lidar surveys have been released openly. Values are heights above the EGM2008 geoid, in metres.

The blend prioritises the highest-resolution available source for each pixel, falls back through a hierarchy of coarser sources to fill voids, and applies seam-line smoothing across mission and survey boundaries so the multi-resolution mosaic stays visually and hydrologically coherent.

What you get

  • A planetary mosaic delivered as 1° × 1° Cloud-Optimized GeoTIFF tiles at the native resolution of each pixel.
  • Companion 30 m and 10 m mosaics for users who want uniform-resolution coverage rather than the highest-available blend.
  • A void mask indicating which pixels were originally missing and required gap-filling.
  • A source-attribution raster indicating which mission or national programme contributed each pixel, and at what native resolution.

Typical uses

  • Watershed delineation and hydrological modelling — finer resolution where it matters most.
  • Urban flood, surface-water and pluvial-runoff modelling in 1 m countries.
  • Visibility, slope and aspect analysis for renewables siting.
  • 3-D terrain visualisation in games, simulators and web maps.
  • Input to landslide, avalanche and infrastructure-risk models.

Notes on resolution

Resolution varies by region and is documented per-pixel in the source-attribution raster. The 1 m coverage broadly tracks countries with open national lidar programmes (much of Europe, North America, parts of Oceania); 10 m coverage extends across additional regions with high-quality national or regional surveys; 30 m is the global baseline elsewhere.

When working with the highest-resolution blend, be aware that pixel size changes across tile and country boundaries — downstream tooling should read the per-tile resolution rather than assume a fixed grid.

Suggested attribution

DEM: OpenData.Earth — CC BY 4.0

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