The analytic TTV signal-to-noise treats the moon’s maximum projected displacement as a cleanly recoverable sinusoid. Real surveys sample the moon’s orbit only at transit epochs, with unknown phase and a possibly tilted orbit — and a fitted transit ephemeris silently absorbs part of the signal. The epoch-level forward model accounts for all of it, and the honest number is what decides whether the dark primary can be confirmed.
from lastmoon.figures.confirmation_frontier import ( frontier_sweep_table, plot_confirmation_frontier,)fig = plot_confirmation_frontier(frontier_sweep_table())fig
The confirmation frontier: where longer baselines and better photometry push the epoch-level TTV SNR past threshold. Conditional on transiting geometry and 100% occurrence; illustrative grid, not a yield.
The forward SNR is a known-period matched-filter statistic: it assumes we know the moon’s orbital period when fitting. A blind period search pays an additional look-elsewhere penalty that is not modeled here — one more reason the threshold matters. The transits themselves are still idealized as central, box-shaped events on a quiet star; both caveats carry into the manuscript.