Modelling acoustic propagation beneath Antarctic sea ice using measured environmental parameters

Autonomous underwater vehicles are improving and expanding in situ observations of sea ice for the validation of satellite remote sensing and climate models. Missions under sea ice, particularly over large distances (up to 100. km) away from the immediate vicinity of a ship or base, require accurate...

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Published in:Deep Sea Research Part II: Topical Studies in Oceanography
Main Authors: Alexander, P., Duncan, Alec, Bose, N., Williams, G.
Format: Article in Journal/Newspaper
Language:unknown
Published: Pergamon 2016
Subjects:
Online Access:https://hdl.handle.net/20.500.11937/4608
https://doi.org/10.1016/j.dsr2.2016.04.026
id ftcurtin:oai:espace.curtin.edu.au:20.500.11937/4608
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spelling ftcurtin:oai:espace.curtin.edu.au:20.500.11937/4608 2023-06-11T04:07:00+02:00 Modelling acoustic propagation beneath Antarctic sea ice using measured environmental parameters Alexander, P. Duncan, Alec Bose, N. Williams, G. 2016 restricted https://hdl.handle.net/20.500.11937/4608 https://doi.org/10.1016/j.dsr2.2016.04.026 unknown Pergamon http://hdl.handle.net/20.500.11937/4608 doi:10.1016/j.dsr2.2016.04.026 Journal Article 2016 ftcurtin https://doi.org/20.500.11937/460810.1016/j.dsr2.2016.04.026 2023-05-30T19:22:13Z Autonomous underwater vehicles are improving and expanding in situ observations of sea ice for the validation of satellite remote sensing and climate models. Missions under sea ice, particularly over large distances (up to 100. km) away from the immediate vicinity of a ship or base, require accurate acoustic communication for monitoring, emergency response and some navigation systems. We investigate the propagation of acoustic signals in the Antarctic seasonal ice zone using the BELLHOP model, examining the influence of ocean and sea ice properties. We processed available observations from around Antarctica to generate input variables such as sound speed, surface reflection coefficient (R) and roughness parameters. The results show that changes in the sound speed profile make the most significant difference to the propagation of the direct path signal. The inclusion of the surface reflected signals from a flat ice surface was found to greatly decrease the transmission loss with range. When ice roughness was added, the transmission loss increased with roughness, in a manner similar to the direct path transmission loss results. The conclusions of this work are that: (1) the accuracy of acoustic modelling in this environment is greatly increased by using realistic sound speed data; (2) a risk averse ranging model would use only the direct path signal transmission; and (3) in a flat ice scenario, much greater ranges can be achieved if the surface reflected transmission paths are included. As autonomous missions under sea ice increase in scale and complexity, it will be increasingly important for operational procedures to include effective modelling of acoustic propagation with representative environmental data. Article in Journal/Newspaper Antarc* Antarctic Antarctica Sea ice Curtin University: espace Antarctic The Antarctic Deep Sea Research Part II: Topical Studies in Oceanography 131 84 95
institution Open Polar
collection Curtin University: espace
op_collection_id ftcurtin
language unknown
description Autonomous underwater vehicles are improving and expanding in situ observations of sea ice for the validation of satellite remote sensing and climate models. Missions under sea ice, particularly over large distances (up to 100. km) away from the immediate vicinity of a ship or base, require accurate acoustic communication for monitoring, emergency response and some navigation systems. We investigate the propagation of acoustic signals in the Antarctic seasonal ice zone using the BELLHOP model, examining the influence of ocean and sea ice properties. We processed available observations from around Antarctica to generate input variables such as sound speed, surface reflection coefficient (R) and roughness parameters. The results show that changes in the sound speed profile make the most significant difference to the propagation of the direct path signal. The inclusion of the surface reflected signals from a flat ice surface was found to greatly decrease the transmission loss with range. When ice roughness was added, the transmission loss increased with roughness, in a manner similar to the direct path transmission loss results. The conclusions of this work are that: (1) the accuracy of acoustic modelling in this environment is greatly increased by using realistic sound speed data; (2) a risk averse ranging model would use only the direct path signal transmission; and (3) in a flat ice scenario, much greater ranges can be achieved if the surface reflected transmission paths are included. As autonomous missions under sea ice increase in scale and complexity, it will be increasingly important for operational procedures to include effective modelling of acoustic propagation with representative environmental data.
format Article in Journal/Newspaper
author Alexander, P.
Duncan, Alec
Bose, N.
Williams, G.
spellingShingle Alexander, P.
Duncan, Alec
Bose, N.
Williams, G.
Modelling acoustic propagation beneath Antarctic sea ice using measured environmental parameters
author_facet Alexander, P.
Duncan, Alec
Bose, N.
Williams, G.
author_sort Alexander, P.
title Modelling acoustic propagation beneath Antarctic sea ice using measured environmental parameters
title_short Modelling acoustic propagation beneath Antarctic sea ice using measured environmental parameters
title_full Modelling acoustic propagation beneath Antarctic sea ice using measured environmental parameters
title_fullStr Modelling acoustic propagation beneath Antarctic sea ice using measured environmental parameters
title_full_unstemmed Modelling acoustic propagation beneath Antarctic sea ice using measured environmental parameters
title_sort modelling acoustic propagation beneath antarctic sea ice using measured environmental parameters
publisher Pergamon
publishDate 2016
url https://hdl.handle.net/20.500.11937/4608
https://doi.org/10.1016/j.dsr2.2016.04.026
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Antarctica
Sea ice
genre_facet Antarc*
Antarctic
Antarctica
Sea ice
op_relation http://hdl.handle.net/20.500.11937/4608
doi:10.1016/j.dsr2.2016.04.026
op_doi https://doi.org/20.500.11937/460810.1016/j.dsr2.2016.04.026
container_title Deep Sea Research Part II: Topical Studies in Oceanography
container_volume 131
container_start_page 84
op_container_end_page 95
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