Polarimetric airborne scientific instrument, mark 2, an ice‐sounding airborne synthetic aperture radar for subglacial 3D imagery
Abstract Polarimetric Airborne Scientific INstrument, mark 2 (PASIN2) is a 150 MHz coherent pulsed radar with the purpose of deep ice sounding for bedrock, subglacial channels and ice‐water interface detection in Antarctica. It is designed and operated by the British Antarctic Survey from 2014. With...
| Published in: | IET Radar, Sonar & Navigation |
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| Main Authors: | , , , , |
| Format: | Article |
| Language: | English |
| Published: |
Wiley
2023-09-01
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| Subjects: | |
| Online Access: | https://doi.org/10.1049/rsn2.12428 |
| _version_ | 1851867656580235264 |
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| author | Álvaro Arenas‐Pingarrón Hugh F. J. Corr Carl Robinson Tom A. Jordan Paul V. Brennan |
| author_facet | Álvaro Arenas‐Pingarrón Hugh F. J. Corr Carl Robinson Tom A. Jordan Paul V. Brennan |
| author_sort | Álvaro Arenas‐Pingarrón |
| collection | DOAJ |
| container_title | IET Radar, Sonar & Navigation |
| description | Abstract Polarimetric Airborne Scientific INstrument, mark 2 (PASIN2) is a 150 MHz coherent pulsed radar with the purpose of deep ice sounding for bedrock, subglacial channels and ice‐water interface detection in Antarctica. It is designed and operated by the British Antarctic Survey from 2014. With multiple antennas, oriented along and across‐track, for transmission and reception, it enables polarimetric 3D estimation of the ice base with a single pass, reducing the gridding density of the survey paths. The off‐line data processing stream consists of channel calibration; 2D synthetic aperture radar (SAR) imaging based on back‐projection, for along‐track and range dimensions; and finally, a direction of arrival estimation (DoA) of the remaining across‐track angle, by modifying the non‐linear MUSIC algorithm. Calibration flights, during the Antarctic Summer campaigns in 16/17 and 19/20 seasons, assessed and validated the instrument and processing performances. Imaging flights over ice streams and ice shelves close to grounding lines demonstrate the 3D sensing capabilities. By resolving directional ambiguities and accounting for reflector across‐track location, the true ice thickness and bed elevation are obtained, thereby removing the error of the usual assumption of vertical DoA, that greatly influence the output of flow models of ice dynamics. |
| format | Article |
| id | doaj-art-309508bd00a248dc99535338e286b3a8 |
| institution | Directory of Open Access Journals |
| issn | 1751-8784 1751-8792 |
| language | English |
| publishDate | 2023-09-01 |
| publisher | Wiley |
| record_format | Article |
| spelling | doaj-art-309508bd00a248dc99535338e286b3a82025-08-19T22:18:01ZengWileyIET Radar, Sonar & Navigation1751-87841751-87922023-09-011791391140410.1049/rsn2.12428Polarimetric airborne scientific instrument, mark 2, an ice‐sounding airborne synthetic aperture radar for subglacial 3D imageryÁlvaro Arenas‐Pingarrón0Hugh F. J. Corr1Carl Robinson2Tom A. Jordan3Paul V. Brennan4British Antarctic Survey Cambridge UKBritish Antarctic Survey Cambridge UKBritish Antarctic Survey Cambridge UKBritish Antarctic Survey Cambridge UKDepartment of Electronic and Electrical Engineering University College London London UKAbstract Polarimetric Airborne Scientific INstrument, mark 2 (PASIN2) is a 150 MHz coherent pulsed radar with the purpose of deep ice sounding for bedrock, subglacial channels and ice‐water interface detection in Antarctica. It is designed and operated by the British Antarctic Survey from 2014. With multiple antennas, oriented along and across‐track, for transmission and reception, it enables polarimetric 3D estimation of the ice base with a single pass, reducing the gridding density of the survey paths. The off‐line data processing stream consists of channel calibration; 2D synthetic aperture radar (SAR) imaging based on back‐projection, for along‐track and range dimensions; and finally, a direction of arrival estimation (DoA) of the remaining across‐track angle, by modifying the non‐linear MUSIC algorithm. Calibration flights, during the Antarctic Summer campaigns in 16/17 and 19/20 seasons, assessed and validated the instrument and processing performances. Imaging flights over ice streams and ice shelves close to grounding lines demonstrate the 3D sensing capabilities. By resolving directional ambiguities and accounting for reflector across‐track location, the true ice thickness and bed elevation are obtained, thereby removing the error of the usual assumption of vertical DoA, that greatly influence the output of flow models of ice dynamics.https://doi.org/10.1049/rsn2.12428airborne radararray signal processingdirection‐of‐arrival estimationMUSIC algorithmremote sensing by radarsynthetic aperture radar |
| spellingShingle | Álvaro Arenas‐Pingarrón Hugh F. J. Corr Carl Robinson Tom A. Jordan Paul V. Brennan Polarimetric airborne scientific instrument, mark 2, an ice‐sounding airborne synthetic aperture radar for subglacial 3D imagery airborne radar array signal processing direction‐of‐arrival estimation MUSIC algorithm remote sensing by radar synthetic aperture radar |
| title | Polarimetric airborne scientific instrument, mark 2, an ice‐sounding airborne synthetic aperture radar for subglacial 3D imagery |
| title_full | Polarimetric airborne scientific instrument, mark 2, an ice‐sounding airborne synthetic aperture radar for subglacial 3D imagery |
| title_fullStr | Polarimetric airborne scientific instrument, mark 2, an ice‐sounding airborne synthetic aperture radar for subglacial 3D imagery |
| title_full_unstemmed | Polarimetric airborne scientific instrument, mark 2, an ice‐sounding airborne synthetic aperture radar for subglacial 3D imagery |
| title_short | Polarimetric airborne scientific instrument, mark 2, an ice‐sounding airborne synthetic aperture radar for subglacial 3D imagery |
| title_sort | polarimetric airborne scientific instrument mark 2 an ice sounding airborne synthetic aperture radar for subglacial 3d imagery |
| topic | airborne radar array signal processing direction‐of‐arrival estimation MUSIC algorithm remote sensing by radar synthetic aperture radar |
| url | https://doi.org/10.1049/rsn2.12428 |
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