Abstract. Observing TeV photons from GRBs can greatly enhance our understanding of their emission mechanisms. Under-sea/ice neutrino telescopes-such as ANTARES in the Mediterranean Sea or IceCube at the South Pole-can also operate as a γ-ray observatory by detecting downgoing muons from the electromagnetic cascade induced by the interaction of the photons with the Earth's atmosphere. Theoretical calculations of the number of detectable muons from single GRB events, located at different redshifts and zenith distances, have been performed. The attenuation by pair production of TeV photons with cosmic infrared background photons has also been included.
Keywords. astroparticle physics, gamma-ray burst: general, elementary particles, methods: analyticalThe ANTARES neutrino telescope is currently operating in the Mediterranean Sea, 40 km offshore Toulon (France) at a depth of 2475 m. With an instrumented volume of ∼ 0.01 km 3 , it is the largest neutrino telescope in the Northern Hemisphere. Although optimized to detect upgoing neutrino-induced muons, it can also detect downgoing photoninduced muons and thus operate as a gamma-ray telescope. Because of its large collecting area, wide field of view, and high duty cycle, there is a potential then for ANTARES to detect TeV photons emitted from gamma-ray burst (GRBs).TeV photons from GRBs are produced from electron Inverse Compton emission or π 0 decay from pγ interactions (Asano & Inoue, 2007). Searching for these photons could help us not only in understanding the mechanisms of GRB emission but also in identifying the possible source of Ultra High-Energy Cosmic Rays (UHECR).Along their path from the source to the Earth, TeV photons interact with ambient IR photons. They annihilate themselves, creating pairs of electron-positron in the process. The transparency of the universe to TeV photons depends on the photons's energy and the distance to the source. Once the surviving TeV photons reach the top of the Earth's atmosphere, they will interact with atmospheric particles and initiate particle showers. Muons are produced from these showers mainly (Halzen et al. 2009) through 1) photoproduction, in which TeV photons interact with atmospheric nuclei and produce pions, followed by the decay of the pion into a positive muon and a muon antineutrino; and 2) direct muon-pair production, where muons are created directly via the channel γ + N → N + µ + + µ − , where N is a nucleus of the atmosphere.Muon production through the first channel dies away with increasing energy, but the cross section of muon-pair production increase with photon energy. At TeV regime it is thus the dominant muon-producing channel. As the muons travels downward toward the detector at the bottom of the sea, they lose their energy through ionization and radiative 321 at https://www.cambridge.org/core/terms. https://doi