Reflections on the anomalous ANITA events: the Antarctic subsurface as a possible explanation

The Antarctic Impulsive Transient Antenna (ANITA) balloon experiment was designed to detect radio signals initiated by high-energy neutrinos and cosmic ray (CR) air showers. These signals are typically discriminated by the polarization and phase inversions of the radio signal. The reflected signal f...

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Published in:Annals of Glaciology
Main Authors: Ian M. Shoemaker, Alexander Kusenko, Peter Kuipers Munneke, Andrew Romero-Wolf, Dustin M. Schroeder, Martin J. Siegert
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2020
Subjects:
Online Access:https://doi.org/10.1017/aog.2020.19
https://doaj.org/article/2df485aba40a4013b3afd3ae6544d9b1
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spelling ftdoajarticles:oai:doaj.org/article:2df485aba40a4013b3afd3ae6544d9b1 2023-05-15T13:29:36+02:00 Reflections on the anomalous ANITA events: the Antarctic subsurface as a possible explanation Ian M. Shoemaker Alexander Kusenko Peter Kuipers Munneke Andrew Romero-Wolf Dustin M. Schroeder Martin J. Siegert 2020-04-01T00:00:00Z https://doi.org/10.1017/aog.2020.19 https://doaj.org/article/2df485aba40a4013b3afd3ae6544d9b1 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0260305520000191/type/journal_article https://doaj.org/toc/0260-3055 https://doaj.org/toc/1727-5644 doi:10.1017/aog.2020.19 0260-3055 1727-5644 https://doaj.org/article/2df485aba40a4013b3afd3ae6544d9b1 Annals of Glaciology, Vol 61, Pp 92-98 (2020) Antarctic glaciology Ice physics Snow physics Meteorology. Climatology QC851-999 article 2020 ftdoajarticles https://doi.org/10.1017/aog.2020.19 2023-03-12T01:31:55Z The Antarctic Impulsive Transient Antenna (ANITA) balloon experiment was designed to detect radio signals initiated by high-energy neutrinos and cosmic ray (CR) air showers. These signals are typically discriminated by the polarization and phase inversions of the radio signal. The reflected signal from CRs suffer phase inversion compared to a direct ‘tau neutrino’ event. In this paper, we study subsurface reflection, which can occur without phase inversion, in the context of the two anomalous up-going events reported by ANITA. It is found that subsurface layers and firn density inversions may plausibly account for the events, while ice fabric layers and wind ablation crusts could also play a role. This hypothesis can be tested with radar surveying of the Antarctic region in the vicinity of the anomalous ANITA events. Future experiments should not use phase inversion as a sole criterion to discriminate between down-going and up-going events, unless the subsurface reflection properties are well understood. Article in Journal/Newspaper Annals of Glaciology Antarc* Antarctic Directory of Open Access Journals: DOAJ Articles Antarctic The Antarctic Annals of Glaciology 61 81 92 98
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Antarctic glaciology
Ice physics
Snow physics
Meteorology. Climatology
QC851-999
spellingShingle Antarctic glaciology
Ice physics
Snow physics
Meteorology. Climatology
QC851-999
Ian M. Shoemaker
Alexander Kusenko
Peter Kuipers Munneke
Andrew Romero-Wolf
Dustin M. Schroeder
Martin J. Siegert
Reflections on the anomalous ANITA events: the Antarctic subsurface as a possible explanation
topic_facet Antarctic glaciology
Ice physics
Snow physics
Meteorology. Climatology
QC851-999
description The Antarctic Impulsive Transient Antenna (ANITA) balloon experiment was designed to detect radio signals initiated by high-energy neutrinos and cosmic ray (CR) air showers. These signals are typically discriminated by the polarization and phase inversions of the radio signal. The reflected signal from CRs suffer phase inversion compared to a direct ‘tau neutrino’ event. In this paper, we study subsurface reflection, which can occur without phase inversion, in the context of the two anomalous up-going events reported by ANITA. It is found that subsurface layers and firn density inversions may plausibly account for the events, while ice fabric layers and wind ablation crusts could also play a role. This hypothesis can be tested with radar surveying of the Antarctic region in the vicinity of the anomalous ANITA events. Future experiments should not use phase inversion as a sole criterion to discriminate between down-going and up-going events, unless the subsurface reflection properties are well understood.
format Article in Journal/Newspaper
author Ian M. Shoemaker
Alexander Kusenko
Peter Kuipers Munneke
Andrew Romero-Wolf
Dustin M. Schroeder
Martin J. Siegert
author_facet Ian M. Shoemaker
Alexander Kusenko
Peter Kuipers Munneke
Andrew Romero-Wolf
Dustin M. Schroeder
Martin J. Siegert
author_sort Ian M. Shoemaker
title Reflections on the anomalous ANITA events: the Antarctic subsurface as a possible explanation
title_short Reflections on the anomalous ANITA events: the Antarctic subsurface as a possible explanation
title_full Reflections on the anomalous ANITA events: the Antarctic subsurface as a possible explanation
title_fullStr Reflections on the anomalous ANITA events: the Antarctic subsurface as a possible explanation
title_full_unstemmed Reflections on the anomalous ANITA events: the Antarctic subsurface as a possible explanation
title_sort reflections on the anomalous anita events: the antarctic subsurface as a possible explanation
publisher Cambridge University Press
publishDate 2020
url https://doi.org/10.1017/aog.2020.19
https://doaj.org/article/2df485aba40a4013b3afd3ae6544d9b1
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Annals of Glaciology
Antarc*
Antarctic
genre_facet Annals of Glaciology
Antarc*
Antarctic
op_source Annals of Glaciology, Vol 61, Pp 92-98 (2020)
op_relation https://www.cambridge.org/core/product/identifier/S0260305520000191/type/journal_article
https://doaj.org/toc/0260-3055
https://doaj.org/toc/1727-5644
doi:10.1017/aog.2020.19
0260-3055
1727-5644
https://doaj.org/article/2df485aba40a4013b3afd3ae6544d9b1
op_doi https://doi.org/10.1017/aog.2020.19
container_title Annals of Glaciology
container_volume 61
container_issue 81
container_start_page 92
op_container_end_page 98
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