Neutrino vertex reconstruction with in-ice radio detectors using surface reflections and implications for the neutrino energy resolution
A. Anker, S. W. Barwick, H. Bernhoff, D. Z. Besson, N. Bingefors, D., Garc\'ia-Fern\'andez, G. Gaswint, C. Glaser, A. Hallgren, J. C. Hanson, S. R., Klein, S. A. Kleinfelder, R. Lahmann, U. Latif, J. Nam, A. Novikov, A., Nelles, M. P. Paul, C. Persichilli, I. Plaisier

TL;DR
This paper proposes a novel method using surface reflections in in-ice radio detectors to reconstruct neutrino vertices and improve energy resolution, supported by simulations and in-situ measurements.
Contribution
It introduces a new technique leveraging surface reflections for neutrino vertex reconstruction and demonstrates its feasibility and impact on energy resolution.
Findings
Time delay correlates with neutrino interaction distance.
Energy resolution contribution is below the inelasticity limit.
In-situ measurements achieve millimeter precision in surface elevation.
Abstract
Ultra high energy neutrinos (eV are efficiently measured via radio signals following a neutrino interaction in ice. An antenna placed (15 m) below the ice surface will measure two signals for the vast majority of events (90% at =eV: a direct pulse and a second delayed pulse from a reflection off the ice surface. This allows for a unique identification of neutrinos against backgrounds arriving from above. Furthermore, the time delay between the direct and reflected signal (D'n'R) correlates with the distance to the neutrino interaction vertex, a crucial quantity to determine the neutrino energy. In a simulation study, we derive the relation between time delay and distance and study the corresponding experimental uncertainties in estimating neutrino energies. We find that the resulting contribution to the energy resolution is well…
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