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Towards a common terminology in radioglaciology
Annals of Glaciology, Volume: 63, Issue: 87-89, Pages: 8 - 12
Swansea University Authors: Bernd Kulessa , Tavi Murray
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DOI (Published version): 10.1017/aog.2023.2
Abstract
Over the past 70 years, many different components of the cryosphere have been imaged with a variety of radar systems using increasingly sophisticated processing techniques. These systems use various pulse lengths, signal frequencies and, in some cases, modulated signals. The increasing diversity of...
Published in: | Annals of Glaciology |
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ISSN: | 0260-3055 1727-5644 |
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Cambridge University Press (CUP)
2022
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URI: | https://cronfa.swan.ac.uk/Record/cronfa65065 |
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v2 65065 2023-11-22 Towards a common terminology in radioglaciology 52acda616e9f6073cbebf497def874c9 0000-0002-4830-4949 Bernd Kulessa Bernd Kulessa true false 8d6e71df690e725cd44191006dac31da 0000-0001-6714-6512 Tavi Murray Tavi Murray true false 2023-11-22 SGE Over the past 70 years, many different components of the cryosphere have been imaged with a variety of radar systems using increasingly sophisticated processing techniques. These systems use various pulse lengths, signal frequencies and, in some cases, modulated signals. The increasing diversity of radar systems has created the potential for confusion due to the use of non-consistent terminology. Here we provide an overview of state-of-the-science radar technologies and suggest a simplified and unified terminology for use by the cryosphere community. We recommend a terminology that is target independent but specifies the characteristics of the signal. Following this recommendation, commercial impulse systems that penetrate the subsurface should be referred to as ground-penetrating radar (GPR), and pulse radars as radio-echo sounding (RES). Continuous-wave (CW) radar systems should be referred to as ground-penetrating CW radars. We further suggest any additional characterisation of the system be expressed using descriptors that specify the platform it is mounted on (e.g. airborne) or the frequency range (e.g. HF (high frequency)) or modulation (e.g. FM (frequency modulated)). Journal Article Annals of Glaciology 63 87-89 8 12 Cambridge University Press (CUP) 0260-3055 1727-5644 Airborne electromagnetic soundings, applied glaciology, glacier geophysics, ground-penetrating radar, radio-echo sounding 30 9 2022 2022-09-30 10.1017/aog.2023.2 http://dx.doi.org/10.1017/aog.2023.2 COLLEGE NANME Geography COLLEGE CODE SGE Swansea University R. Schlegel is funded by the IMPACT operation fellowship, which has been part-funded by the European Regional Development Fund through the Welsh Government and Swansea University. This work was supported by NERC AFI award numbers NE/G014159/1, NE/G013187/1 and NE/F015879/1. 2023-12-13T14:11:22.9722574 2023-11-22T09:14:29.7872958 Faculty of Science and Engineering School of Biosciences, Geography and Physics - Geography Rebecca Schlegel 1 Bernd Kulessa 0000-0002-4830-4949 2 Tavi Murray 0000-0001-6714-6512 3 Olaf Eisen 0000-0002-6380-962x 4 65065__29259__74a85bbc36084793bfe09c7b46ea3b8a.pdf 65065.VOR.pdf 2023-12-13T14:09:51.9230054 Output 632435 application/pdf Version of Record true © The Author(s), 2023. Published by Cambridge University Press on behalf of The International Glaciological Society. Distributed under the terms of a Creative Commons Attribution 4.0 International License (CC BY 4.0). true eng https://creativecommons.org/licenses/by/4.0/ |
title |
Towards a common terminology in radioglaciology |
spellingShingle |
Towards a common terminology in radioglaciology Bernd Kulessa Tavi Murray |
title_short |
Towards a common terminology in radioglaciology |
title_full |
Towards a common terminology in radioglaciology |
title_fullStr |
Towards a common terminology in radioglaciology |
title_full_unstemmed |
Towards a common terminology in radioglaciology |
title_sort |
Towards a common terminology in radioglaciology |
author_id_str_mv |
52acda616e9f6073cbebf497def874c9 8d6e71df690e725cd44191006dac31da |
author_id_fullname_str_mv |
52acda616e9f6073cbebf497def874c9_***_Bernd Kulessa 8d6e71df690e725cd44191006dac31da_***_Tavi Murray |
author |
Bernd Kulessa Tavi Murray |
author2 |
Rebecca Schlegel Bernd Kulessa Tavi Murray Olaf Eisen |
format |
Journal article |
container_title |
Annals of Glaciology |
container_volume |
63 |
container_issue |
87-89 |
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8 |
publishDate |
2022 |
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Swansea University |
issn |
0260-3055 1727-5644 |
doi_str_mv |
10.1017/aog.2023.2 |
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Cambridge University Press (CUP) |
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Faculty of Science and Engineering |
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Faculty of Science and Engineering |
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School of Biosciences, Geography and Physics - Geography{{{_:::_}}}Faculty of Science and Engineering{{{_:::_}}}School of Biosciences, Geography and Physics - Geography |
url |
http://dx.doi.org/10.1017/aog.2023.2 |
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description |
Over the past 70 years, many different components of the cryosphere have been imaged with a variety of radar systems using increasingly sophisticated processing techniques. These systems use various pulse lengths, signal frequencies and, in some cases, modulated signals. The increasing diversity of radar systems has created the potential for confusion due to the use of non-consistent terminology. Here we provide an overview of state-of-the-science radar technologies and suggest a simplified and unified terminology for use by the cryosphere community. We recommend a terminology that is target independent but specifies the characteristics of the signal. Following this recommendation, commercial impulse systems that penetrate the subsurface should be referred to as ground-penetrating radar (GPR), and pulse radars as radio-echo sounding (RES). Continuous-wave (CW) radar systems should be referred to as ground-penetrating CW radars. We further suggest any additional characterisation of the system be expressed using descriptors that specify the platform it is mounted on (e.g. airborne) or the frequency range (e.g. HF (high frequency)) or modulation (e.g. FM (frequency modulated)). |
published_date |
2022-09-30T14:11:23Z |
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11.016235 |