Describe the geodesic variation by a smooth map , with each curve a timelike geodesic parametrized by proper time. Its tangent vector is and its deviation vector is . Thus measures the first-order separation of neighboring members at the same value of proper time.
Mixed coordinate derivatives on the parameter surface commute. Consequently, along the variation,For an embedded two-dimensional variation this is the usual Lie bracket of vector fields on its image; more generally the same identity is read along the map using its commuting parameter derivatives. Since the Levi-Civita connection is torsion-free, it follows that .
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