In situ estimation of ice crystal properties at the South Pole using LED calibration data from the IceCube Neutrino Observatory ...

The IceCube Neutrino Observatory instruments about 1 km3 of deep, glacial ice at the geographic South Pole. It uses 5160 photomultipliers to detect Cherenkov light emitted by charged relativistic particles. An unexpected light propagation effect observed by the experiment is an anisotropic attenuati...

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Main Authors: Abbasi, Rasha, Ackermann, Markus, Adams, Jenni, Aggarwal, Nakul, Aguilar, Juanan, Ahlers, Markus, Ahrens, Maryon, Alameddine, Jean-Marco, Alves Junior, Antonio Augusto, Amin, Najia Moureen Binte, Andeen, Karen, Anderson, Tyler, Anton, Gisela, Argüelles, Carlos, Ashida, Yosuke, Athanasiadou, Sofia, Axani, Spencer, Bai, Xinhua, Balagopal V, Aswathi, Baricevic, Moreno, Barwick, Steve, Basu, Vedant, Bay, Ryan, Beatty, James, Becker, Karl Heinz, Becker Tjus, Julia, Beise, Jakob, Bellenghi, Chiara, Benda, Samuel, BenZvi, Segev, Berley, David, Bernardini, Elisa, Besson, Dave, Binder, Gary, Bindig, Daniel, Blaufuss, Erik, Blot, Summer, Bontempo, Federico, Book, Julia, Borowka, Jürgen, Boscolo Meneguolo, Caterina, Böser, Sebastian, Botner, Olga, Böttcher, Jakob, Bourbeau, Etienne, Braun, Jim, Brinson, Bennett, Brostean-Kaiser, Jannes, Burley, Ryan, Busse, Raffaela
Format: Text
Language:English
Published: Copernicus Publications 2024
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Online Access:https://dx.doi.org/10.5445/ir/1000168626
https://publikationen.bibliothek.kit.edu/1000168626
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Summary:The IceCube Neutrino Observatory instruments about 1 km3 of deep, glacial ice at the geographic South Pole. It uses 5160 photomultipliers to detect Cherenkov light emitted by charged relativistic particles. An unexpected light propagation effect observed by the experiment is an anisotropic attenuation, which is aligned with the local flow direction of the ice. We examine birefringent light propaga- tion through the polycrystalline ice microstructure as a pos- sible explanation for this effect. The predictions of a first- principles model developed for this purpose, in particular curved light trajectories resulting from asymmetric diffusion, provide a qualitatively good match to the main features of the data. This in turn allows us to deduce ice crystal properties. Since the wavelength of the detected light is short compared to the crystal size, these crystal properties include not only the crystal orientation fabric, but also the average crystal size and shape, as a function of depth. By adding small empiri- ...