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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Main Author: Elliott, John M.
Other Authors: NAVAL POSTGRADUATE SCHOOL MONTEREY CA
Format: Text
Language:English
Published: 1992
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA256723
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA256723
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spelling 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
institution Open Polar
collection 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.
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