Airborne River-Ice Thickness Profiling with Helicopter-Borne UHF Short-Pulse Radar

Abstract The ice-thickness profiling performance of a helicopter-mounted short-pulse radar operating at approximate center frequencies of 600 and 900 MHz was assessed. The antenna packages were mounted 1.2 m off the skid of a small helicopter whose speed and altitude were varied from about 1.8 to 9...

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Published in:Journal of Glaciology
Main Authors: Arcone, Steven A, Delaney, Allan J
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1987
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000008923
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000008923
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spelling crcambridgeupr:10.1017/s0022143000008923 2024-03-03T08:46:04+00:00 Airborne River-Ice Thickness Profiling with Helicopter-Borne UHF Short-Pulse Radar Arcone, Steven A Delaney, Allan J 1987 http://dx.doi.org/10.1017/s0022143000008923 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000008923 en eng Cambridge University Press (CUP) Journal of Glaciology volume 33, issue 115, page 330-340 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1987 crcambridgeupr https://doi.org/10.1017/s0022143000008923 2024-02-08T08:36:10Z Abstract The ice-thickness profiling performance of a helicopter-mounted short-pulse radar operating at approximate center frequencies of 600 and 900 MHz was assessed. The antenna packages were mounted 1.2 m off the skid of a small helicopter whose speed and altitude were varied from about 1.8 to 9 m/s and 3 to 12 m. Clutter from the helicopter offered minimal interference with the ice data. Data were acquired in Alaska over lakes (as a proving exercise) and two rivers, whose conditions varied from open water to over 1.5 m of solid ice with numerous frazil-ice formations. The most readily interpretable data were acquired when the ice or snow surface was smooth. Detailed surface investigations on the Tanana River revealed good correlations of echo delay with solid ice depth, but an insensitivity to frazil-ice depth due to its high water content. On the Yukon River, coinciding temporally coherent surface and bottom reflections were associated with solid ice and smooth surfaces. All cases of incoherent surface returns (scatter) occurred over ice rubble. Rough-surface scattering was always followed by the appearance of bottom scattering but, in many cases, including a hanging-wall formation of solid frazil ice, bottom scattering occurred beneath coherent, smooth-surface reflections. Areas of incoherent bottom scattering investigated by drilling revealed highly variable ice conditions, including frazil ice. The minimum ice thickness that could be resolved from the raw data was about 0.2 m with the 600 MHz antenna and less than 0.15 m with the 900 MHz antenna. Article in Journal/Newspaper Journal of Glaciology Yukon river Alaska Yukon Cambridge University Press Yukon Journal of Glaciology 33 115 330 340
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Arcone, Steven A
Delaney, Allan J
Airborne River-Ice Thickness Profiling with Helicopter-Borne UHF Short-Pulse Radar
topic_facet Earth-Surface Processes
description Abstract The ice-thickness profiling performance of a helicopter-mounted short-pulse radar operating at approximate center frequencies of 600 and 900 MHz was assessed. The antenna packages were mounted 1.2 m off the skid of a small helicopter whose speed and altitude were varied from about 1.8 to 9 m/s and 3 to 12 m. Clutter from the helicopter offered minimal interference with the ice data. Data were acquired in Alaska over lakes (as a proving exercise) and two rivers, whose conditions varied from open water to over 1.5 m of solid ice with numerous frazil-ice formations. The most readily interpretable data were acquired when the ice or snow surface was smooth. Detailed surface investigations on the Tanana River revealed good correlations of echo delay with solid ice depth, but an insensitivity to frazil-ice depth due to its high water content. On the Yukon River, coinciding temporally coherent surface and bottom reflections were associated with solid ice and smooth surfaces. All cases of incoherent surface returns (scatter) occurred over ice rubble. Rough-surface scattering was always followed by the appearance of bottom scattering but, in many cases, including a hanging-wall formation of solid frazil ice, bottom scattering occurred beneath coherent, smooth-surface reflections. Areas of incoherent bottom scattering investigated by drilling revealed highly variable ice conditions, including frazil ice. The minimum ice thickness that could be resolved from the raw data was about 0.2 m with the 600 MHz antenna and less than 0.15 m with the 900 MHz antenna.
format Article in Journal/Newspaper
author Arcone, Steven A
Delaney, Allan J
author_facet Arcone, Steven A
Delaney, Allan J
author_sort Arcone, Steven A
title Airborne River-Ice Thickness Profiling with Helicopter-Borne UHF Short-Pulse Radar
title_short Airborne River-Ice Thickness Profiling with Helicopter-Borne UHF Short-Pulse Radar
title_full Airborne River-Ice Thickness Profiling with Helicopter-Borne UHF Short-Pulse Radar
title_fullStr Airborne River-Ice Thickness Profiling with Helicopter-Borne UHF Short-Pulse Radar
title_full_unstemmed Airborne River-Ice Thickness Profiling with Helicopter-Borne UHF Short-Pulse Radar
title_sort airborne river-ice thickness profiling with helicopter-borne uhf short-pulse radar
publisher Cambridge University Press (CUP)
publishDate 1987
url http://dx.doi.org/10.1017/s0022143000008923
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000008923
geographic Yukon
geographic_facet Yukon
genre Journal of Glaciology
Yukon river
Alaska
Yukon
genre_facet Journal of Glaciology
Yukon river
Alaska
Yukon
op_source Journal of Glaciology
volume 33, issue 115, page 330-340
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000008923
container_title Journal of Glaciology
container_volume 33
container_issue 115
container_start_page 330
op_container_end_page 340
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