Probing the angular and polarization reconstruction of the ARIANNA detector at the South Pole

• Main Authors: Anker, A, Barwick, SW, Bernhoff, H, Besson, DZ, Bingefors, N, García-Fernández, D, Gaswint, G, Glaser, C, Hallgren, A, Hanson, JC, Klein, SR, Kleinfelder, SA, Lahmann, R, Latif, U, Meyers, ZS, Nam, J, Novikov, A, Nelles, A, Paul, MP, Persichilli, C, Plaisier, I, Tatar, J, Wang, S-H, Welling, C
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: eScholarship, University of California 2020
• Subjects: Data analysis; Performance of High Energy Physics Detectors; Systematic effects; Neutrino detectors; astro-ph.IM; Physical Sciences; Engineering; Nuclear & Particles Physics; Antarctic; South Pole; Antarc*; ice core; South pole
• Online Access: https://escholarship.org/uc/item/44c3358z

The sources of ultra-high energy (UHE) cosmic rays, which can have energies up to 1020 eV, remain a mystery. UHE neutrinos may provide important clues to understanding the nature of cosmic-ray sources. ARIANNA aims to detect UHE neutrinos via radio (Askaryan) emission from particle showers when a neutrino interacts with ice, which is an efficient method for neutrinos with energies between 1016 eV and 1020 eV. The ARIANNA radio detectors are located in Antarctic ice just beneath the surface. Neutrino observation requires that radio pulses propagate to the antennas at the surface with minimum distortion by the ice and firn medium. Using the residual hole from the South Pole Ice Core Project, radio pulses were emitted from a transmitter located up to 1.7 km below the snow surface. By measuring these signals with an ARIANNA surface station, the angular and polarization reconstruction abilities are quantified, which are required to measure the direction of the neutrino. After deconvolving the raw signals for the detector response and attenuation from propagation through the ice, the signal pulses show no significant distortion and agree with a reference measurement of the emitter made in an anechoic chamber. Furthermore, the signal pulses reveal no significant birefringence for our tested geometry of mostly vertical ice propagation. The origin of the transmitted radio pulse was measured with an angular resolution of 0.37◦ indicating that the neutrino direction can be determined with good precision if the polarization of the radio-pulse can be well determined. In the present study we obtained a resolution of the polarization vector of 2.7◦. Neither measurement show a significant offset relative to expectation.