Sea surface height anomaly, one year
Deep Water · 00:30 · 2026
If the ocean were still and unbroken by land, its surface would follow the geoid, an equipotential surface shaped by the uneven pull of Earth's mass. Shown here to true scale, then exaggerated.
Watch for the moment the exaggeration begins. At true scale the shape cannot be seen at all; the highs and lows appear only once the relief is multiplied.