Use negative-exponential spatial Fourier transforms and finite-time spectral boundary transforms:
Write and . Integrate the local relation first over and then over time. The left and right endpoint fluxes have opposite signs, giving the finite-interval Airy global relation
All these spatial and temporal integral transforms are entire functions of for sufficiently smooth data on the finite intervals. Put and , . The dispersion relation obeys ; hence the same global relation holds at all three . In particular, the missing traces satisfy the concrete linear system
where, with a common upper time limit ,
The finite-time spectral boundary transforms are invariant under these rotations because their time kernel depends only on . The coefficients multiplying them are not invariant; these differences make the three equations useful for eliminating the missing boundary traces.