Polarization Angle Dependence of Vertically Propagating Radio-Frequency Signals in South Polar Ice
To better understand the effect of ice properties on the science reach of radio experiments designed to measure ultrahigh energy neutrinos (UHEN), we recently considered the timing and amplitude characteristics of radio-frequency (RF) signals propagating along multi-kilometer, primarily horizontal t...
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ftunivnebraskali:oai:digitalcommons.unl.edu:physicsfacpub-1354 2023-11-12T04:03:20+01:00 Polarization Angle Dependence of Vertically Propagating Radio-Frequency Signals in South Polar Ice Bensson, DaveZ Kravchenko, Ilya Nivedita, Krishna 2022-08-15T07:00:00Z application/pdf https://digitalcommons.unl.edu/physicsfacpub/355 https://digitalcommons.unl.edu/context/physicsfacpub/article/1354/viewcontent/Beeson_AP_2023_Polarization_Angle_Dependence.pdf unknown DigitalCommons@University of Nebraska - Lincoln https://digitalcommons.unl.edu/physicsfacpub/355 https://digitalcommons.unl.edu/context/physicsfacpub/article/1354/viewcontent/Beeson_AP_2023_Polarization_Angle_Dependence.pdf Faculty Publications, Department of Physics and Astronomy Physical Sciences and Mathematics Physics text 2022 ftunivnebraskali 2023-10-30T12:10:12Z To better understand the effect of ice properties on the science reach of radio experiments designed to measure ultrahigh energy neutrinos (UHEN), we recently considered the timing and amplitude characteristics of radio-frequency (RF) signals propagating along multi-kilometer, primarily horizontal trajectories through cold Polar ice at the South Pole. That analysis indicated satisfactory agreement with a model of ice birefringence based on ice crystal (ĉ-axis) data culled from the South Pole Ice Core Experiment (SPICE). Here we explore the geometrically complementary case of signals propagating along primarily vertical trajectories, using extant data from the Askaryan Radio Array (ARA) experiment, supplemented by a refined analysis of older RICE experimental data. The timing characteristics of the South Polar data are in general agreement with the same birefringence model, although a several nanosecond discrepancy is found in comparison to Taylor Dome data. Re-analysis of older RICE data also confirm the correlation of signal amplitudes reflected from internal-layers with the direction of ice flow, similar to previous observations made along a traverse from Dome Fuji to the Antarctic coast. These results have two important implications for radio-based UHEN experiments: i) if birefringence can be locally calibrated, the timing characteristics of signals propagating from neutrino-ice interactions to a distant receiver might be used to infer the distance-to-vertex, which is necessary to estimate the energy of the progenitor neutrino, ii) the measured reflectivity of internal layers may result in previously-unanticipated backgrounds to UHEN searches, requiring significantly more modeling and analysis. Text Antarc* Antarctic ice core South pole South pole University of Nebraska-Lincoln: DigitalCommons@UNL Antarctic Dome Fuji ENVELOPE(39.700,39.700,-77.317,-77.317) South Pole Taylor Dome ENVELOPE(157.667,157.667,-77.667,-77.667) The Antarctic |
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University of Nebraska-Lincoln: DigitalCommons@UNL |
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ftunivnebraskali |
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Physical Sciences and Mathematics Physics |
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Physical Sciences and Mathematics Physics Bensson, DaveZ Kravchenko, Ilya Nivedita, Krishna Polarization Angle Dependence of Vertically Propagating Radio-Frequency Signals in South Polar Ice |
topic_facet |
Physical Sciences and Mathematics Physics |
description |
To better understand the effect of ice properties on the science reach of radio experiments designed to measure ultrahigh energy neutrinos (UHEN), we recently considered the timing and amplitude characteristics of radio-frequency (RF) signals propagating along multi-kilometer, primarily horizontal trajectories through cold Polar ice at the South Pole. That analysis indicated satisfactory agreement with a model of ice birefringence based on ice crystal (ĉ-axis) data culled from the South Pole Ice Core Experiment (SPICE). Here we explore the geometrically complementary case of signals propagating along primarily vertical trajectories, using extant data from the Askaryan Radio Array (ARA) experiment, supplemented by a refined analysis of older RICE experimental data. The timing characteristics of the South Polar data are in general agreement with the same birefringence model, although a several nanosecond discrepancy is found in comparison to Taylor Dome data. Re-analysis of older RICE data also confirm the correlation of signal amplitudes reflected from internal-layers with the direction of ice flow, similar to previous observations made along a traverse from Dome Fuji to the Antarctic coast. These results have two important implications for radio-based UHEN experiments: i) if birefringence can be locally calibrated, the timing characteristics of signals propagating from neutrino-ice interactions to a distant receiver might be used to infer the distance-to-vertex, which is necessary to estimate the energy of the progenitor neutrino, ii) the measured reflectivity of internal layers may result in previously-unanticipated backgrounds to UHEN searches, requiring significantly more modeling and analysis. |
format |
Text |
author |
Bensson, DaveZ Kravchenko, Ilya Nivedita, Krishna |
author_facet |
Bensson, DaveZ Kravchenko, Ilya Nivedita, Krishna |
author_sort |
Bensson, DaveZ |
title |
Polarization Angle Dependence of Vertically Propagating Radio-Frequency Signals in South Polar Ice |
title_short |
Polarization Angle Dependence of Vertically Propagating Radio-Frequency Signals in South Polar Ice |
title_full |
Polarization Angle Dependence of Vertically Propagating Radio-Frequency Signals in South Polar Ice |
title_fullStr |
Polarization Angle Dependence of Vertically Propagating Radio-Frequency Signals in South Polar Ice |
title_full_unstemmed |
Polarization Angle Dependence of Vertically Propagating Radio-Frequency Signals in South Polar Ice |
title_sort |
polarization angle dependence of vertically propagating radio-frequency signals in south polar ice |
publisher |
DigitalCommons@University of Nebraska - Lincoln |
publishDate |
2022 |
url |
https://digitalcommons.unl.edu/physicsfacpub/355 https://digitalcommons.unl.edu/context/physicsfacpub/article/1354/viewcontent/Beeson_AP_2023_Polarization_Angle_Dependence.pdf |
long_lat |
ENVELOPE(39.700,39.700,-77.317,-77.317) ENVELOPE(157.667,157.667,-77.667,-77.667) |
geographic |
Antarctic Dome Fuji South Pole Taylor Dome The Antarctic |
geographic_facet |
Antarctic Dome Fuji South Pole Taylor Dome The Antarctic |
genre |
Antarc* Antarctic ice core South pole South pole |
genre_facet |
Antarc* Antarctic ice core South pole South pole |
op_source |
Faculty Publications, Department of Physics and Astronomy |
op_relation |
https://digitalcommons.unl.edu/physicsfacpub/355 https://digitalcommons.unl.edu/context/physicsfacpub/article/1354/viewcontent/Beeson_AP_2023_Polarization_Angle_Dependence.pdf |
_version_ |
1782336910324137984 |