A three-dimensional calculation of atmospheric neutrinos
G. D. Barr, T. K. Gaisser, P. Lipari, S. Robbins, T. Stanev
TL;DR
This work advances atmospheric neutrino flux modeling by implementing a fully three-dimensional Monte Carlo calculation that includes geomagnetic bending of secondaries and backtracking-based geomagnetic cutoffs. By systematically comparing 3D and traditional 1D approaches, the authors demonstrate that 1D is adequate above roughly 5 GeV, with only small azimuthal differences at high energies and notable horizon-related effects at low energies. The paper details a fast, flexible pipeline with a flat detector approximation, binlet weighting to control fluctuations, and modular decay/interaction generators, enabling precise quantification of 3D effects and guiding when the more complex 3D treatment is essential. These results are important for the accurate interpretation of atmospheric neutrino oscillation analyses and for refining oscillation parameter extractions in neutrino experiments.
Abstract
A Monte-Carlo calculation of the atmospheric neutrino fluxes [1,2] has been extended to take account of the three-dimensional (3D) nature of the problem, including the bending of secondary particles in the geomagnetic field. Emphasis has been placed on minimizing the approximations when introducing the 3D considerations. In this paper, we describe the techniques used and quantify the effects of the small approximations which remain. We compare 3D and 1D calculations using the same physics input in order to evaluate the conditions under which the 3D calculation is required and when the considerably simpler 1D calculation is adequate. We find that the 1D and 3D results are essentially identical for neutrino energy greater than 5 GeV except for small effects in the azimuthal distributions due to bending of the secondary muon by the geomagnetic field during their propagation in the atmosphere.
