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

• 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: Article in Journal/Newspaper
• Language: unknown
• Published: arXiv 2022
• Subjects: Instrumentation and Methods for Astrophysics astro-ph.IM; High Energy Astrophysical Phenomena astro-ph.HE; High Energy Physics - Experiment hep-ex; FOS Physical sciences; Greenland
• Online Access: https://dx.doi.org/10.48550/arxiv.2201.07846; https://arxiv.org/abs/2201.07846

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 $L_α$. We find an approximately linear dependence of $L_α$ on frequency with the best fit of the average field attenuation for the upper 1500 m of ice: $\langle L_α\rangle = \big( (1024 \pm 50) - (0.65 \pm 0.06) (ν/$MHz$)\big)$ m for frequencies $ν\in [145 - 350]$ MHz. : 12 pages, 8 figures, submitted to Journal of Glaciology