The third SETI channel — after radio and optical. Neutrinos cross 17,900 light-years without scattering, absorption, or deflection. The question is whether a directed beam carries enough flux to beat IceCube's background.
Neutrino flux 1/r². Vertical lines: IceCube detection threshold (dashed amber) and ωCen distance (solid teal). Horizontal dashed line: atmospheric νμ background in 1 yr at selected detector volume.
| Detector | Volume | Events/yr | S/B ratio | Status |
|---|
Physics model: A directed muon-neutrino beam of power P_tx (watts) at energy E_ν (eV) produces a neutrino flux at Earth of Φ = P_tx / (4π d² E_ν), where d = 5.49 kpc for ωCen. The detection rate is N = Φ × σ(E_ν) × ρ_ice × V_eff, where σ(E_ν) ≈ 6.7×10⁻³⁹ cm² × (E_ν/GeV) is the neutrino–nucleon charged-current cross-section, ρ_ice ≈ 0.917 g/cm³, and V_eff is the effective detector volume. Atmospheric background: ~100 muon neutrino events per year per km³ above 1 TeV (IceCube measurement).
Beam directionality: A real neutrino source from a muon collider would have a divergence of ~1 mrad (Anchordoqui et al. 2008). This model assumes perfect beam alignment toward Earth — an optimistic assumption. A randomly oriented beam reduces the effective flux by (solid angle factor), making detection far harder. The 1/4πd² factor used here implicitly assumes isotropic emission; a directed beam would be brighter by the beaming factor.
Background: The atmospheric neutrino background at IceCube is approximately 100,000 events/year at >100 GeV, falling to ~100/year at >1 TeV and ~1/year at >100 TeV. The astrophysical diffuse background discovered by IceCube (2013) adds ~10–50 events/year above 100 TeV. A directed SETI signal would need to exceed this background either by rate or by source localisation.
OCS IceCube proposal: The OCS IceCube proposal targets astrophysical neutrino emission from the ωCen IMBH region — not a SETI signal, but the same detector that would catch a deliberate beam. See proposal_icecube.html for the astrophysical case.
References: Anchordoqui et al. 2008 (arXiv:0803.0409) · IceCube 2013 Science 342:1242856 · Learned & Pakvasa 1995 Astropart. Phys. 3:267