Mapping of gravity strength and sea surface height can actually be used to work backwards to find the shape of the sea floor; if there’s a big underwater mountain, there’s likely to be a small bump in the ocean surface just above it, as water is gravitationally attracted towards its rocky bulk. This ocean surface shape is independent of waves and currents and weather, and it’s called the geoid.1331 ↱
The Blue Machine
Helen Czerski