Simulation of Acoustic Multipath Arrival Structure in the Barents Sea
In support of the Barents Sea Polar Front Experiment (BSPFEX) in September 1992 (Barents Sea Polar Front Group, 1992), the planned 224 Hz tomography signal transmissions from a near bottom sound source to a vertical receiver array consisting of 16 hydrophones were simulated. Acoustic rays were trace...
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ftdtic:ADA256723 2023-05-15T15:38:04+02:00 Simulation of Acoustic Multipath Arrival Structure in the Barents Sea Elliott, John M. NAVAL POSTGRADUATE SCHOOL MONTEREY CA 1992-06 text/html http://www.dtic.mil/docs/citations/ADA256723 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA256723 en eng http://www.dtic.mil/docs/citations/ADA256723 Approved for public release; distribution is unlimited. DTIC AND NTIS Physical and Dynamic Oceanography Holography Acoustics *ACOUSTIC ARRAYS *TOMOGRAPHY *UNDERWATER ACOUSTICS *MULTIPATH TRANSMISSION *OCEAN ENVIRONMENTS VELOCITY INPUT ENVIRONMENTS STRUCTURES ARRAYS OCEANS BOTTOM LOSS OMNIDIRECTIONAL OCEANOGRAPHY PLANE WAVES BOTTOM BARENTS SEA ARRIVAL HYDROPHONES LOSSES SOUND SURFACES SIGNALS RECEIVERS BEAM FORMING Text 1992 ftdtic 2016-02-22T12:18:28Z In support of the Barents Sea Polar Front Experiment (BSPFEX) in September 1992 (Barents Sea Polar Front Group, 1992), the planned 224 Hz tomography signal transmissions from a near bottom sound source to a vertical receiver array consisting of 16 hydrophones were simulated. Acoustic rays were traced to the receiver array at a range of 50 km using the NOAA Hamiltonian Raytracing Program for the Ocean (HARPO). Input to HARPO was a mathematical ocean environment based on historical bathymetric and sound speed data. Acoustic multipath arrival structure was constructed through eigenray searches and estimation of raytube spreading and surface and bottom losses. A resolvability analysis of the simulated arrival structure reveals that there are a total of 49 unique resolvable ray arrivals. Among them; 42 are from individual omnidirectional hydrophones and 7 from plane wave beamforming. Acoustic Tomography, Ocean Acoustics, Oceanography, Barents Sea. Text Barents Sea Defense Technical Information Center: DTIC Technical Reports database Barents Sea |
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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 |
Physical and Dynamic Oceanography Holography Acoustics *ACOUSTIC ARRAYS *TOMOGRAPHY *UNDERWATER ACOUSTICS *MULTIPATH TRANSMISSION *OCEAN ENVIRONMENTS VELOCITY INPUT ENVIRONMENTS STRUCTURES ARRAYS OCEANS BOTTOM LOSS OMNIDIRECTIONAL OCEANOGRAPHY PLANE WAVES BOTTOM BARENTS SEA ARRIVAL HYDROPHONES LOSSES SOUND SURFACES SIGNALS RECEIVERS BEAM FORMING |
spellingShingle |
Physical and Dynamic Oceanography Holography Acoustics *ACOUSTIC ARRAYS *TOMOGRAPHY *UNDERWATER ACOUSTICS *MULTIPATH TRANSMISSION *OCEAN ENVIRONMENTS VELOCITY INPUT ENVIRONMENTS STRUCTURES ARRAYS OCEANS BOTTOM LOSS OMNIDIRECTIONAL OCEANOGRAPHY PLANE WAVES BOTTOM BARENTS SEA ARRIVAL HYDROPHONES LOSSES SOUND SURFACES SIGNALS RECEIVERS BEAM FORMING Elliott, John M. Simulation of Acoustic Multipath Arrival Structure in the Barents Sea |
topic_facet |
Physical and Dynamic Oceanography Holography Acoustics *ACOUSTIC ARRAYS *TOMOGRAPHY *UNDERWATER ACOUSTICS *MULTIPATH TRANSMISSION *OCEAN ENVIRONMENTS VELOCITY INPUT ENVIRONMENTS STRUCTURES ARRAYS OCEANS BOTTOM LOSS OMNIDIRECTIONAL OCEANOGRAPHY PLANE WAVES BOTTOM BARENTS SEA ARRIVAL HYDROPHONES LOSSES SOUND SURFACES SIGNALS RECEIVERS BEAM FORMING |
description |
In support of the Barents Sea Polar Front Experiment (BSPFEX) in September 1992 (Barents Sea Polar Front Group, 1992), the planned 224 Hz tomography signal transmissions from a near bottom sound source to a vertical receiver array consisting of 16 hydrophones were simulated. Acoustic rays were traced to the receiver array at a range of 50 km using the NOAA Hamiltonian Raytracing Program for the Ocean (HARPO). Input to HARPO was a mathematical ocean environment based on historical bathymetric and sound speed data. Acoustic multipath arrival structure was constructed through eigenray searches and estimation of raytube spreading and surface and bottom losses. A resolvability analysis of the simulated arrival structure reveals that there are a total of 49 unique resolvable ray arrivals. Among them; 42 are from individual omnidirectional hydrophones and 7 from plane wave beamforming. Acoustic Tomography, Ocean Acoustics, Oceanography, Barents Sea. |
author2 |
NAVAL POSTGRADUATE SCHOOL MONTEREY CA |
format |
Text |
author |
Elliott, John M. |
author_facet |
Elliott, John M. |
author_sort |
Elliott, John M. |
title |
Simulation of Acoustic Multipath Arrival Structure in the Barents Sea |
title_short |
Simulation of Acoustic Multipath Arrival Structure in the Barents Sea |
title_full |
Simulation of Acoustic Multipath Arrival Structure in the Barents Sea |
title_fullStr |
Simulation of Acoustic Multipath Arrival Structure in the Barents Sea |
title_full_unstemmed |
Simulation of Acoustic Multipath Arrival Structure in the Barents Sea |
title_sort |
simulation of acoustic multipath arrival structure in the barents sea |
publishDate |
1992 |
url |
http://www.dtic.mil/docs/citations/ADA256723 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA256723 |
geographic |
Barents Sea |
geographic_facet |
Barents Sea |
genre |
Barents Sea |
genre_facet |
Barents Sea |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA256723 |
op_rights |
Approved for public release; distribution is unlimited. |
_version_ |
1766368764500115456 |