HF/VHF Radar Sounding of Ice from Manned and Unmanned Airborne Platforms

Ice thickness and bed topography of fast-flowing outlet glaciers are large sources of uncertainty for the current ice sheet models used to predict future contributions to sea-level rise. Due to a lack of coverage and difficulty in sounding and imaging with ice-penetrating radars, these regions remai...

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Published in:Geosciences
Main Authors: Emily Arnold, Fernando Rodriguez-Morales, John Paden, Carl Leuschen, Shawn Keshmiri, Stephen Yan, Mark Ewing, Rick Hale, Ali Mahmood, Aaron Blevins, Akhilesh Mishra, Teja Karidi, Bailey Miller, John Sonntag
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2018
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Online Access:https://doi.org/10.3390/geosciences8050182
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spelling ftmdpi:oai:mdpi.com:/2076-3263/8/5/182/ 2023-08-20T04:05:55+02:00 HF/VHF Radar Sounding of Ice from Manned and Unmanned Airborne Platforms Emily Arnold Fernando Rodriguez-Morales John Paden Carl Leuschen Shawn Keshmiri Stephen Yan Mark Ewing Rick Hale Ali Mahmood Aaron Blevins Akhilesh Mishra Teja Karidi Bailey Miller John Sonntag agris 2018-05-16 application/pdf https://doi.org/10.3390/geosciences8050182 EN eng Multidisciplinary Digital Publishing Institute Geophysics https://dx.doi.org/10.3390/geosciences8050182 https://creativecommons.org/licenses/by/4.0/ Geosciences; Volume 8; Issue 5; Pages: 182 remote sensing ice sheets glaciers radar unmanned aircraft system (UAS) synthetic aperture radar (SAR) Text 2018 ftmdpi https://doi.org/10.3390/geosciences8050182 2023-07-31T21:31:30Z Ice thickness and bed topography of fast-flowing outlet glaciers are large sources of uncertainty for the current ice sheet models used to predict future contributions to sea-level rise. Due to a lack of coverage and difficulty in sounding and imaging with ice-penetrating radars, these regions remain poorly constrained in models. Increases in off-nadir scattering due to the highly crevassed surfaces, volumetric scattering (due to debris and/or pockets of liquid water), and signal attenuation (due to warmer ice near the bottom) are all impediments in detecting bed-echoes. A set of high-frequency (HF)/very high-frequency (VHF) radars operating at 14 MHz and 30–35 MHz were developed at the University of Kansas to sound temperate ice and outlet glaciers. We have deployed these radars on a small unmanned aircraft system (UAS) and a DHC-6 Twin Otter. For both installations, the system utilized a dipole antenna oriented in the cross-track direction, providing some performance advantages over other temperate ice sounders operating at lower frequencies. In this paper, we describe the platform-sensor systems, field operations, data-processing techniques, and preliminary results. We also compare our results with data from other ice-sounding radars that operate at frequencies both above (Center for Remote Sensing of Ice Sheets (CReSIS) Multichannel Coherent Depth Sounder (MCoRDS)) and below (Jet Propulsion Laboratory (JPL) Warm Ice Sounding Explorer (WISE)) our HF/VHF system. During field campaigns, both unmanned and manned platforms flew closely spaced parallel and repeat flight lines. We examine these data sets to determine image coherency between flight lines and discuss the feasibility of forming 2D synthetic apertures by using such a mission approach. Text Center for Remote Sensing of Ice Sheets (CReSIS) Ice Sheet MDPI Open Access Publishing Geosciences 8 5 182
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic remote sensing
ice sheets
glaciers
radar
unmanned aircraft system (UAS)
synthetic aperture radar (SAR)
spellingShingle remote sensing
ice sheets
glaciers
radar
unmanned aircraft system (UAS)
synthetic aperture radar (SAR)
Emily Arnold
Fernando Rodriguez-Morales
John Paden
Carl Leuschen
Shawn Keshmiri
Stephen Yan
Mark Ewing
Rick Hale
Ali Mahmood
Aaron Blevins
Akhilesh Mishra
Teja Karidi
Bailey Miller
John Sonntag
HF/VHF Radar Sounding of Ice from Manned and Unmanned Airborne Platforms
topic_facet remote sensing
ice sheets
glaciers
radar
unmanned aircraft system (UAS)
synthetic aperture radar (SAR)
description Ice thickness and bed topography of fast-flowing outlet glaciers are large sources of uncertainty for the current ice sheet models used to predict future contributions to sea-level rise. Due to a lack of coverage and difficulty in sounding and imaging with ice-penetrating radars, these regions remain poorly constrained in models. Increases in off-nadir scattering due to the highly crevassed surfaces, volumetric scattering (due to debris and/or pockets of liquid water), and signal attenuation (due to warmer ice near the bottom) are all impediments in detecting bed-echoes. A set of high-frequency (HF)/very high-frequency (VHF) radars operating at 14 MHz and 30–35 MHz were developed at the University of Kansas to sound temperate ice and outlet glaciers. We have deployed these radars on a small unmanned aircraft system (UAS) and a DHC-6 Twin Otter. For both installations, the system utilized a dipole antenna oriented in the cross-track direction, providing some performance advantages over other temperate ice sounders operating at lower frequencies. In this paper, we describe the platform-sensor systems, field operations, data-processing techniques, and preliminary results. We also compare our results with data from other ice-sounding radars that operate at frequencies both above (Center for Remote Sensing of Ice Sheets (CReSIS) Multichannel Coherent Depth Sounder (MCoRDS)) and below (Jet Propulsion Laboratory (JPL) Warm Ice Sounding Explorer (WISE)) our HF/VHF system. During field campaigns, both unmanned and manned platforms flew closely spaced parallel and repeat flight lines. We examine these data sets to determine image coherency between flight lines and discuss the feasibility of forming 2D synthetic apertures by using such a mission approach.
format Text
author Emily Arnold
Fernando Rodriguez-Morales
John Paden
Carl Leuschen
Shawn Keshmiri
Stephen Yan
Mark Ewing
Rick Hale
Ali Mahmood
Aaron Blevins
Akhilesh Mishra
Teja Karidi
Bailey Miller
John Sonntag
author_facet Emily Arnold
Fernando Rodriguez-Morales
John Paden
Carl Leuschen
Shawn Keshmiri
Stephen Yan
Mark Ewing
Rick Hale
Ali Mahmood
Aaron Blevins
Akhilesh Mishra
Teja Karidi
Bailey Miller
John Sonntag
author_sort Emily Arnold
title HF/VHF Radar Sounding of Ice from Manned and Unmanned Airborne Platforms
title_short HF/VHF Radar Sounding of Ice from Manned and Unmanned Airborne Platforms
title_full HF/VHF Radar Sounding of Ice from Manned and Unmanned Airborne Platforms
title_fullStr HF/VHF Radar Sounding of Ice from Manned and Unmanned Airborne Platforms
title_full_unstemmed HF/VHF Radar Sounding of Ice from Manned and Unmanned Airborne Platforms
title_sort hf/vhf radar sounding of ice from manned and unmanned airborne platforms
publisher Multidisciplinary Digital Publishing Institute
publishDate 2018
url https://doi.org/10.3390/geosciences8050182
op_coverage agris
genre Center for Remote Sensing of Ice Sheets (CReSIS)
Ice Sheet
genre_facet Center for Remote Sensing of Ice Sheets (CReSIS)
Ice Sheet
op_source Geosciences; Volume 8; Issue 5; Pages: 182
op_relation Geophysics
https://dx.doi.org/10.3390/geosciences8050182
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/geosciences8050182
container_title Geosciences
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