FRAM II Single Channel Ambient Noise Statistics: A Paper Presented at the 101st Meeting of the Acoustical Society of America, 19 May 1981, Ottawa, Canada.
This document describes the results of a statistical analysis study of FRAM II arctic under-ice ambient noise data. The specific data that were analyzed were recorded on 23-24 April 1980 from a pack ice camp in the Arctic Ocean, located at 86 deg N latitude, 25 deg W longitude. At this location, the...
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ftdtic:ADA108755 2023-05-15T14:46:36+02:00 FRAM II Single Channel Ambient Noise Statistics: A Paper Presented at the 101st Meeting of the Acoustical Society of America, 19 May 1981, Ottawa, Canada. Dwyer,Roger F NAVAL UNDERWATER SYSTEMS CENTER NEW LONDON CT NEW LONDON LAB 1981-11-25 text/html http://www.dtic.mil/docs/citations/ADA108755 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA108755 en eng http://www.dtic.mil/docs/citations/ADA108755 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost Acoustics *AMBIENT NOISE *UNDERWATER ACOUSTICS *PACK ICE FREQUENCY TENSILE STRESS STATISTICAL ANALYSIS IMPULSE NOISE FRICTION SPECTRUM ANALYSIS TIME DOMAIN ACOUSTIC DATA COLLISIONS DEEP OCEANS ARCTIC OCEAN UNDERICE Non-Gaussian noise Shorefast ice Ice dynamics LPN-NUSC-A-750- 30 PE61152N Text 1981 ftdtic 2016-02-20T21:07:52Z This document describes the results of a statistical analysis study of FRAM II arctic under-ice ambient noise data. The specific data that were analyzed were recorded on 23-24 April 1980 from a pack ice camp in the Arctic Ocean, located at 86 deg N latitude, 25 deg W longitude. At this location, the bottom depth was approximately 4000 m. The measurement system consisted of a broadband omnidirectional hydrophone, suspended to a depth of 91 m from a sonobuoy located in a lead. Under the influence of arctic currents, the pack ice was slowly moving. This movement caused rifting and cracking of ice, which occurred, at times, throughout the experiments and represented a structured acoustic noise source. Both impulsive and burst noise were identified in the data and were probably created by tensile cracks and rubbing ice masses. Text Arctic Arctic Ocean Ice permafrost Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean Canada |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Snow Ice and Permafrost Acoustics *AMBIENT NOISE *UNDERWATER ACOUSTICS *PACK ICE FREQUENCY TENSILE STRESS STATISTICAL ANALYSIS IMPULSE NOISE FRICTION SPECTRUM ANALYSIS TIME DOMAIN ACOUSTIC DATA COLLISIONS DEEP OCEANS ARCTIC OCEAN UNDERICE Non-Gaussian noise Shorefast ice Ice dynamics LPN-NUSC-A-750- 30 PE61152N |
spellingShingle |
Snow Ice and Permafrost Acoustics *AMBIENT NOISE *UNDERWATER ACOUSTICS *PACK ICE FREQUENCY TENSILE STRESS STATISTICAL ANALYSIS IMPULSE NOISE FRICTION SPECTRUM ANALYSIS TIME DOMAIN ACOUSTIC DATA COLLISIONS DEEP OCEANS ARCTIC OCEAN UNDERICE Non-Gaussian noise Shorefast ice Ice dynamics LPN-NUSC-A-750- 30 PE61152N Dwyer,Roger F FRAM II Single Channel Ambient Noise Statistics: A Paper Presented at the 101st Meeting of the Acoustical Society of America, 19 May 1981, Ottawa, Canada. |
topic_facet |
Snow Ice and Permafrost Acoustics *AMBIENT NOISE *UNDERWATER ACOUSTICS *PACK ICE FREQUENCY TENSILE STRESS STATISTICAL ANALYSIS IMPULSE NOISE FRICTION SPECTRUM ANALYSIS TIME DOMAIN ACOUSTIC DATA COLLISIONS DEEP OCEANS ARCTIC OCEAN UNDERICE Non-Gaussian noise Shorefast ice Ice dynamics LPN-NUSC-A-750- 30 PE61152N |
description |
This document describes the results of a statistical analysis study of FRAM II arctic under-ice ambient noise data. The specific data that were analyzed were recorded on 23-24 April 1980 from a pack ice camp in the Arctic Ocean, located at 86 deg N latitude, 25 deg W longitude. At this location, the bottom depth was approximately 4000 m. The measurement system consisted of a broadband omnidirectional hydrophone, suspended to a depth of 91 m from a sonobuoy located in a lead. Under the influence of arctic currents, the pack ice was slowly moving. This movement caused rifting and cracking of ice, which occurred, at times, throughout the experiments and represented a structured acoustic noise source. Both impulsive and burst noise were identified in the data and were probably created by tensile cracks and rubbing ice masses. |
author2 |
NAVAL UNDERWATER SYSTEMS CENTER NEW LONDON CT NEW LONDON LAB |
format |
Text |
author |
Dwyer,Roger F |
author_facet |
Dwyer,Roger F |
author_sort |
Dwyer,Roger F |
title |
FRAM II Single Channel Ambient Noise Statistics: A Paper Presented at the 101st Meeting of the Acoustical Society of America, 19 May 1981, Ottawa, Canada. |
title_short |
FRAM II Single Channel Ambient Noise Statistics: A Paper Presented at the 101st Meeting of the Acoustical Society of America, 19 May 1981, Ottawa, Canada. |
title_full |
FRAM II Single Channel Ambient Noise Statistics: A Paper Presented at the 101st Meeting of the Acoustical Society of America, 19 May 1981, Ottawa, Canada. |
title_fullStr |
FRAM II Single Channel Ambient Noise Statistics: A Paper Presented at the 101st Meeting of the Acoustical Society of America, 19 May 1981, Ottawa, Canada. |
title_full_unstemmed |
FRAM II Single Channel Ambient Noise Statistics: A Paper Presented at the 101st Meeting of the Acoustical Society of America, 19 May 1981, Ottawa, Canada. |
title_sort |
fram ii single channel ambient noise statistics: a paper presented at the 101st meeting of the acoustical society of america, 19 may 1981, ottawa, canada. |
publishDate |
1981 |
url |
http://www.dtic.mil/docs/citations/ADA108755 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA108755 |
geographic |
Arctic Arctic Ocean Canada |
geographic_facet |
Arctic Arctic Ocean Canada |
genre |
Arctic Arctic Ocean Ice permafrost |
genre_facet |
Arctic Arctic Ocean Ice permafrost |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA108755 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766317800661450752 |