The relative acceleration of neighboring freely falling bodies is measured by geodesic deviation, comparing their infinitesimal separation in a parallel transport frame along a reference timelike geodesic with tangent . With defined by the covariant derivative commutator, it has the displayed form. In the Newtonian limit the corresponding tidal tensor is the spatial gradient of the gravitational acceleration. A single freely falling body can remove local gravitational acceleration by its frame choice, whereas relative tidal acceleration measures curvature.
Use signature , and . For a weak stationary metric, the Christoffel symbol satisfies to first order. Differentiation gives the displayed Riemann curvature tensor component; products of connections are second order. For it is . Its radial eigenvalue is negative and its transverse eigenvalues positive, giving radial stretching and transverse compression in the geodesic deviation equation with a positive curvature term on the left.

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Tidal acceleration refers to the gradual increase in the rotational period of a celestial body, such as a planet or moon, due to the gravitational interaction with another nearby body. This phenomenon is primarily observed in the context of the Earth-Moon system and the Earth-Sun system. In the case of the Earth and Moon, the gravitational pull of the Moon creates tides in the Earth's oceans.