Short Range Acoustic Propagation Under Arctic Ice Cover During Icex 16

During the Arctic Submarine LabHosted 2016 Ice Exercise, short-range acoustic propagation under ice cover was evaluated. Sound speed profiles were measured and a series of acoustic signals at depths of 25, 50, and 183 meters and frequencies of 950, 2800, and 4050 hertz, respectively, were transmitte...

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Bibliographic Details
Main Author: Nelson,Michael S
Other Authors: NAVAL POSTGRADUATE SCHOOL MONTEREY CA MONTEREY United States
Format: Text
Language:English
Published: 2016
Subjects:
Online Access:http://www.dtic.mil/docs/citations/AD1029872
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD1029872
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spelling ftdtic:AD1029872 2023-05-15T14:35:29+02:00 Short Range Acoustic Propagation Under Arctic Ice Cover During Icex 16 Nelson,Michael S NAVAL POSTGRADUATE SCHOOL MONTEREY CA MONTEREY United States 2016-09-01 text/html http://www.dtic.mil/docs/citations/AD1029872 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD1029872 en eng http://www.dtic.mil/docs/citations/AD1029872 Approved For Public Release; ACOUSTIC PROPAGATION transmission loss arctic ocean Arctic Beaufort Sea sound speed profile bellhop modeling Short Range Arctic Ice Cover variable layer ARCTIC OCEANOGRAPHIC Ray Paths Text 2016 ftdtic 2017-04-23T14:47:11Z During the Arctic Submarine LabHosted 2016 Ice Exercise, short-range acoustic propagation under ice cover was evaluated. Sound speed profiles were measured and a series of acoustic signals at depths of 25, 50, and 183 meters and frequencies of 950, 2800, and 4050 hertz, respectively, were transmitted from the ice camp. Remotely located vertical line arrays at ranges of approximately 1.5 and 3 kilometers recorded the transmissions. The sound speed profile data obtained at the ice camp were used to model ray paths and transmission loss in the observed frequency, range, and depth combinations. The received signals were processed and analyzed to determine observed variability and transmission loss, which was then compared to the models. A key finding was the presence of a highly variable layer at 50 meters, which was characterized by its effects on sound signals and the sound speed profile. Observations also highlighted variability during transmissions and between trials while finding significant weaknesses in the modeling softwares ability to accurately predict the acoustic environment in the region. Text Arctic Arctic Ocean Beaufort Sea Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic ACOUSTIC PROPAGATION
transmission loss
arctic ocean
Arctic
Beaufort Sea
sound speed profile
bellhop
modeling
Short Range
Arctic Ice Cover
variable layer
ARCTIC OCEANOGRAPHIC
Ray Paths
spellingShingle ACOUSTIC PROPAGATION
transmission loss
arctic ocean
Arctic
Beaufort Sea
sound speed profile
bellhop
modeling
Short Range
Arctic Ice Cover
variable layer
ARCTIC OCEANOGRAPHIC
Ray Paths
Nelson,Michael S
Short Range Acoustic Propagation Under Arctic Ice Cover During Icex 16
topic_facet ACOUSTIC PROPAGATION
transmission loss
arctic ocean
Arctic
Beaufort Sea
sound speed profile
bellhop
modeling
Short Range
Arctic Ice Cover
variable layer
ARCTIC OCEANOGRAPHIC
Ray Paths
description During the Arctic Submarine LabHosted 2016 Ice Exercise, short-range acoustic propagation under ice cover was evaluated. Sound speed profiles were measured and a series of acoustic signals at depths of 25, 50, and 183 meters and frequencies of 950, 2800, and 4050 hertz, respectively, were transmitted from the ice camp. Remotely located vertical line arrays at ranges of approximately 1.5 and 3 kilometers recorded the transmissions. The sound speed profile data obtained at the ice camp were used to model ray paths and transmission loss in the observed frequency, range, and depth combinations. The received signals were processed and analyzed to determine observed variability and transmission loss, which was then compared to the models. A key finding was the presence of a highly variable layer at 50 meters, which was characterized by its effects on sound signals and the sound speed profile. Observations also highlighted variability during transmissions and between trials while finding significant weaknesses in the modeling softwares ability to accurately predict the acoustic environment in the region.
author2 NAVAL POSTGRADUATE SCHOOL MONTEREY CA MONTEREY United States
format Text
author Nelson,Michael S
author_facet Nelson,Michael S
author_sort Nelson,Michael S
title Short Range Acoustic Propagation Under Arctic Ice Cover During Icex 16
title_short Short Range Acoustic Propagation Under Arctic Ice Cover During Icex 16
title_full Short Range Acoustic Propagation Under Arctic Ice Cover During Icex 16
title_fullStr Short Range Acoustic Propagation Under Arctic Ice Cover During Icex 16
title_full_unstemmed Short Range Acoustic Propagation Under Arctic Ice Cover During Icex 16
title_sort short range acoustic propagation under arctic ice cover during icex 16
publishDate 2016
url http://www.dtic.mil/docs/citations/AD1029872
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD1029872
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Beaufort Sea
genre_facet Arctic
Arctic Ocean
Beaufort Sea
op_relation http://www.dtic.mil/docs/citations/AD1029872
op_rights Approved For Public Release;
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