Acoustic Mode Coherence in the Arctic Ocean
The dual issues of modal decomposition for tonal sound fields and the temporal coherence of the modal amplitudes are investigated for the case of the central Arctic sound channel at very low frequencies (15-80 Hz). The performance of each of four different modal beamforming algorithms when applied t...
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ftdtic:ADA216942 2023-05-15T14:38:46+02:00 Acoustic Mode Coherence in the Arctic Ocean Polcari, John J. MASSACHUSETTS INST OF TECH CAMBRIDGE 1986-05 text/html http://www.dtic.mil/docs/citations/ADA216942 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA216942 en eng http://www.dtic.mil/docs/citations/ADA216942 Approved for public release; distribution is unlimited. DTIC AND NTIS Acoustic Detection and Detectors Acoustics *ACOUSTIC ARRAYS *BEAM FORMING MEASUREMENT STATISTICS COHERENCE SURFACE ROUGHNESS EFFICIENCY THESES PROCESSING EQUIPMENT SENSITIVITY ICE LIMITATIONS LEAST SQUARES METHOD ATTENUATION PERTURBATIONS ACOUSTIC SCATTERING DRAG AMPLITUDE DECOMPOSITION HYDRODYNAMICS ACOUSTIC DATA CHANNELS MULTIPLE BEAMS(RADIATION) ARCTIC REGIONS AUDIO TONES UNDERWATER SOUND SIGNALS LOW FREQUENCIES ARCTIC OCEAN ACOUSTIC CHANNELS ALGORITHMS TIME INTERVALS MODAL DECOMPOSITION Text 1986 ftdtic 2016-02-22T23:44:04Z The dual issues of modal decomposition for tonal sound fields and the temporal coherence of the modal amplitudes are investigated for the case of the central Arctic sound channel at very low frequencies (15-80 Hz). The performance of each of four different modal beamforming algorithms when applied to the vertical array deployed during the FRAM IV Arctic Acoustic Experiment is analyzed. A multiple beam (or decoupled beam) least squares processor produces the most acceptable results for Arctic conditions. The modal decomposition is sensitive to vertical array tilt caused by hydrodynamic drag; a technique for its estimation from the acoustic data is developed. Tonal data taken from both the horizontal and vertical arrays deployed during FRAM IV is analyzed. Horizontal array results confirm the modal amplitudes generated from vertical array data. The rough surface scattering from the ice canopy places an upper limit of 40 Hz on efficient surface duct propagation. Attenuation measurements for the first mode show excellent agreement with predictions made for ice scattering using the method of small perturbations and experimental ice statistics. The high levels of coherence observed (0.95 to 0.99) show that tonal signal propagation in the Arctic channel is essentially deterministic for time periods well in excess of one hour. Theses. Original contains color plates: All DTIC reproductions will be in black and white. Text Arctic Arctic Ocean Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean Arctic Sound ENVELOPE(-108.852,-108.852,67.534,67.534) |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Acoustic Detection and Detectors Acoustics *ACOUSTIC ARRAYS *BEAM FORMING MEASUREMENT STATISTICS COHERENCE SURFACE ROUGHNESS EFFICIENCY THESES PROCESSING EQUIPMENT SENSITIVITY ICE LIMITATIONS LEAST SQUARES METHOD ATTENUATION PERTURBATIONS ACOUSTIC SCATTERING DRAG AMPLITUDE DECOMPOSITION HYDRODYNAMICS ACOUSTIC DATA CHANNELS MULTIPLE BEAMS(RADIATION) ARCTIC REGIONS AUDIO TONES UNDERWATER SOUND SIGNALS LOW FREQUENCIES ARCTIC OCEAN ACOUSTIC CHANNELS ALGORITHMS TIME INTERVALS MODAL DECOMPOSITION |
spellingShingle |
Acoustic Detection and Detectors Acoustics *ACOUSTIC ARRAYS *BEAM FORMING MEASUREMENT STATISTICS COHERENCE SURFACE ROUGHNESS EFFICIENCY THESES PROCESSING EQUIPMENT SENSITIVITY ICE LIMITATIONS LEAST SQUARES METHOD ATTENUATION PERTURBATIONS ACOUSTIC SCATTERING DRAG AMPLITUDE DECOMPOSITION HYDRODYNAMICS ACOUSTIC DATA CHANNELS MULTIPLE BEAMS(RADIATION) ARCTIC REGIONS AUDIO TONES UNDERWATER SOUND SIGNALS LOW FREQUENCIES ARCTIC OCEAN ACOUSTIC CHANNELS ALGORITHMS TIME INTERVALS MODAL DECOMPOSITION Polcari, John J. Acoustic Mode Coherence in the Arctic Ocean |
topic_facet |
Acoustic Detection and Detectors Acoustics *ACOUSTIC ARRAYS *BEAM FORMING MEASUREMENT STATISTICS COHERENCE SURFACE ROUGHNESS EFFICIENCY THESES PROCESSING EQUIPMENT SENSITIVITY ICE LIMITATIONS LEAST SQUARES METHOD ATTENUATION PERTURBATIONS ACOUSTIC SCATTERING DRAG AMPLITUDE DECOMPOSITION HYDRODYNAMICS ACOUSTIC DATA CHANNELS MULTIPLE BEAMS(RADIATION) ARCTIC REGIONS AUDIO TONES UNDERWATER SOUND SIGNALS LOW FREQUENCIES ARCTIC OCEAN ACOUSTIC CHANNELS ALGORITHMS TIME INTERVALS MODAL DECOMPOSITION |
description |
The dual issues of modal decomposition for tonal sound fields and the temporal coherence of the modal amplitudes are investigated for the case of the central Arctic sound channel at very low frequencies (15-80 Hz). The performance of each of four different modal beamforming algorithms when applied to the vertical array deployed during the FRAM IV Arctic Acoustic Experiment is analyzed. A multiple beam (or decoupled beam) least squares processor produces the most acceptable results for Arctic conditions. The modal decomposition is sensitive to vertical array tilt caused by hydrodynamic drag; a technique for its estimation from the acoustic data is developed. Tonal data taken from both the horizontal and vertical arrays deployed during FRAM IV is analyzed. Horizontal array results confirm the modal amplitudes generated from vertical array data. The rough surface scattering from the ice canopy places an upper limit of 40 Hz on efficient surface duct propagation. Attenuation measurements for the first mode show excellent agreement with predictions made for ice scattering using the method of small perturbations and experimental ice statistics. The high levels of coherence observed (0.95 to 0.99) show that tonal signal propagation in the Arctic channel is essentially deterministic for time periods well in excess of one hour. Theses. Original contains color plates: All DTIC reproductions will be in black and white. |
author2 |
MASSACHUSETTS INST OF TECH CAMBRIDGE |
format |
Text |
author |
Polcari, John J. |
author_facet |
Polcari, John J. |
author_sort |
Polcari, John J. |
title |
Acoustic Mode Coherence in the Arctic Ocean |
title_short |
Acoustic Mode Coherence in the Arctic Ocean |
title_full |
Acoustic Mode Coherence in the Arctic Ocean |
title_fullStr |
Acoustic Mode Coherence in the Arctic Ocean |
title_full_unstemmed |
Acoustic Mode Coherence in the Arctic Ocean |
title_sort |
acoustic mode coherence in the arctic ocean |
publishDate |
1986 |
url |
http://www.dtic.mil/docs/citations/ADA216942 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA216942 |
long_lat |
ENVELOPE(-108.852,-108.852,67.534,67.534) |
geographic |
Arctic Arctic Ocean Arctic Sound |
geographic_facet |
Arctic Arctic Ocean Arctic Sound |
genre |
Arctic Arctic Ocean |
genre_facet |
Arctic Arctic Ocean |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA216942 |
op_rights |
Approved for public release; distribution is unlimited. |
_version_ |
1766310788094492672 |