In situ, broadband measurement of the radio frequency attenuation length at Summit Station, Greenland

Over the last 25 years, radiowave detection of neutrino-generated signals, using cold polar ice as the neutrino target, has emerged as perhaps the most promising technique for detection of extragalactic ultra-high energy neutrinos (corresponding to neutrino energies in excess of 0.01 Joules, or $10^...

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Main Authors: Aguilar, J. A, Allison, P, Beatty, J. J, Besson, D, Bishop, A, Botner, O, Bouma, S, Buitink, S, Cataldo, M, Clark, B. A, Curtis-Ginsberg, Z, Connolly, A, Dasgupta, P, de Kockere, S, de Vries, K. D, Deaconu, C, DuVernois, M. A, Glaser, C, Hallgren, A, Hallmann, S, Hanson, J. C, Hendricks, B, Hornhuber, C, Hughes, K, Karle, A, Kelley, J. L, Kravchenko, I, Krebs, R, Lahmann, R, Latif, U, Mammo, J, Meyers, Z. S, Michaels, K, Mulrey, K, Nelles, A, Novikov, A, Nozdrina, A, Oberla, E, Oeyen, B, Pan, Y, Pandya, H, Plaisier, I, Punsuebsay, N, Pyras, L, Ryckbosch, D, Scholten, O, Seckel, D, Seikh, M. F. H, Smith, D, Southall, D, Torres, J, Toscano, S, Tosi, D, Broeck, D. J. Van Den, van Eijndhoven, N, Vieregg, A. G, Welling, C, Williams, D. R, Wissel, S, Young, R, Zink, A
Format: Journal Article
Language:English
Published: 02-08-2022
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Summary:Over the last 25 years, radiowave detection of neutrino-generated signals, using cold polar ice as the neutrino target, has emerged as perhaps the most promising technique for detection of extragalactic ultra-high energy neutrinos (corresponding to neutrino energies in excess of 0.01 Joules, or $10^{17}$ electron volts). During the summer of 2021 and in tandem with the initial deployment of the Radio Neutrino Observatory in Greenland (RNO-G), we conducted radioglaciological measurements at Summit Station, Greenland to refine our understanding of the ice target. We report the result of one such measurement, the radio-frequency electric field attenuation length $L_\alpha$. We find an approximately linear dependence of $L_\alpha$ on frequency with the best fit of the average field attenuation for the upper 1500 m of ice: $\langle L_\alpha \rangle = \big( (1154 \pm 121) - (0.81 \pm 0.14) (\nu/$MHz$)\big)$ m for frequencies $\nu \in [145 - 350]$ MHz.
DOI:10.48550/arxiv.2201.07846