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...

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Published in:IET Radar, Sonar & Navigation
Main Authors: Álvaro Arenas‐Pingarrón, Hugh F. J. Corr, Carl Robinson, Tom A. Jordan, Paul V. Brennan
Format: Article
Language:English
Published: Wiley 2023-09-01
Subjects:
Online Access:https://doi.org/10.1049/rsn2.12428
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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.
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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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