Cosmological soft-graviton consistency relation Created 2026-09-28 Updated 2026-11-05
A sufficiently long adiabatic tensor mode acts locally as an anisotropic change of spatial coordinates. Write the spatial metric as , with transverse and trace-free. Removing a constant long mode maps the short wavevector to at first order. The trace-free deformation has no first-order volume Jacobian, so its effect on an isotropic scalar power spectrum is
Correlating this response with the long graviton gives
The prime removes the momentum-conserving , and is the power of the same polarization amplitude used in . Thus polarization normalization must be consistent on both sides.[ref]
This consistency relation concerns a squeezed bispectrum configuration: it relates a three-point correlation function to a coordinate response of a two-point function. It requires the long tensor to be adiabatic and the state/dynamics to respect that response. Additional physical long-wavelength effects or incompatible initial-state assumptions cannot simply be replaced by this identity.
The background spatial metric is . For the large spatial diffeomorphism
homogeneity and isotropy imply that the purely spatial background Christoffel symbols vanish. Hence
The shift is constant, transverse and traceless, and is therefore the zero-momentum adiabatic tensor mode.
A scalar transforms by its Lie derivative:
Fourier transformation and integration by parts in momentum space give
The term proportional to vanishes because the deformation is traceless.
Applying the scalar transformation from part i to both fields gives
The derivative of the Dirac delta distribution is proportional to and vanishes after contraction with traceless . Removing that delta function leaves
Equating the two sides of the Ward-Takahashi identity and resolving the soft graviton into a polarization yields the cosmological soft-graviton consistency relation
For an isotropic power spectrum this is equivalently
The long-wavelength adiabatic tensor mode acts on the short two-point function as an anisotropic rescaling of its momentum.