SW06 Data Analysis, Slope-Canyon Experiment Planning, and Long-Range Sound Propagation with Applications to the Arctic

The long term goals of our shallow water acoustics work are to: 1) understand the nature of low frequency (10-1500 Hz) acoustic propagation and scattering in shallow water when strong oceanic variability is present in the form of fronts, eddies, boundary layers, and internal waves and 2) begin plann...

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Main Author: Lynch, James F
Other Authors: WOODS HOLE OCEANOGRAPHIC INSTITUTION MA
Format: Text
Language:English
Published: 2011
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA571750
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA571750
id ftdtic:ADA571750
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spelling ftdtic:ADA571750 2023-05-15T15:05:41+02:00 SW06 Data Analysis, Slope-Canyon Experiment Planning, and Long-Range Sound Propagation with Applications to the Arctic Lynch, James F WOODS HOLE OCEANOGRAPHIC INSTITUTION MA 2011-09 text/html http://www.dtic.mil/docs/citations/ADA571750 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA571750 en eng http://www.dtic.mil/docs/citations/ADA571750 Approved for public release; distribution is unlimited. DTIC Physical and Dynamic Oceanography Acoustics *BOUNDARY LAYER *FRONTS(OCEANOGRAPHY) *INTERNAL WAVES *LOW FREQUENCY *SHALLOW WATER *UNDERWATER ACOUSTICS ACOUSTIC SCATTERING ACOUSTIC WAVES CANYONS DEEP WATER EDDIES(FLUID MECHANICS) LONG RANGE(DISTANCE) NUMERICAL ANALYSIS PROPAGATION SLOPE SOUND TRANSMISSION THREE DIMENSIONAL Text 2011 ftdtic 2016-02-24T10:05:03Z The long term goals of our shallow water acoustics work are to: 1) understand the nature of low frequency (10-1500 Hz) acoustic propagation and scattering in shallow water when strong oceanic variability is present in the form of fronts, eddies, boundary layers, and internal waves and 2) begin planning a 2016 field experiment to look at the complicated boundary between deep and shallow water, i.e. the slope/canyon region. Our primary objectives this year were: 1) to continue the analysis of the vast data set collected by the SW06 experiment, model it with theory and numerical models, and publish the results in a JASA Special Issue. 3-D acoustics and oceanographic effects were of particular interest. 2) Begin 2016 experimental planning, both on an individual basis, and in conjunction with the whole ocean acoustics community. Text Arctic Defense Technical Information Center: DTIC Technical Reports database Arctic
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Physical and Dynamic Oceanography
Acoustics
*BOUNDARY LAYER
*FRONTS(OCEANOGRAPHY)
*INTERNAL WAVES
*LOW FREQUENCY
*SHALLOW WATER
*UNDERWATER ACOUSTICS
ACOUSTIC SCATTERING
ACOUSTIC WAVES
CANYONS
DEEP WATER
EDDIES(FLUID MECHANICS)
LONG RANGE(DISTANCE)
NUMERICAL ANALYSIS
PROPAGATION
SLOPE
SOUND TRANSMISSION
THREE DIMENSIONAL
spellingShingle Physical and Dynamic Oceanography
Acoustics
*BOUNDARY LAYER
*FRONTS(OCEANOGRAPHY)
*INTERNAL WAVES
*LOW FREQUENCY
*SHALLOW WATER
*UNDERWATER ACOUSTICS
ACOUSTIC SCATTERING
ACOUSTIC WAVES
CANYONS
DEEP WATER
EDDIES(FLUID MECHANICS)
LONG RANGE(DISTANCE)
NUMERICAL ANALYSIS
PROPAGATION
SLOPE
SOUND TRANSMISSION
THREE DIMENSIONAL
Lynch, James F
SW06 Data Analysis, Slope-Canyon Experiment Planning, and Long-Range Sound Propagation with Applications to the Arctic
topic_facet Physical and Dynamic Oceanography
Acoustics
*BOUNDARY LAYER
*FRONTS(OCEANOGRAPHY)
*INTERNAL WAVES
*LOW FREQUENCY
*SHALLOW WATER
*UNDERWATER ACOUSTICS
ACOUSTIC SCATTERING
ACOUSTIC WAVES
CANYONS
DEEP WATER
EDDIES(FLUID MECHANICS)
LONG RANGE(DISTANCE)
NUMERICAL ANALYSIS
PROPAGATION
SLOPE
SOUND TRANSMISSION
THREE DIMENSIONAL
description The long term goals of our shallow water acoustics work are to: 1) understand the nature of low frequency (10-1500 Hz) acoustic propagation and scattering in shallow water when strong oceanic variability is present in the form of fronts, eddies, boundary layers, and internal waves and 2) begin planning a 2016 field experiment to look at the complicated boundary between deep and shallow water, i.e. the slope/canyon region. Our primary objectives this year were: 1) to continue the analysis of the vast data set collected by the SW06 experiment, model it with theory and numerical models, and publish the results in a JASA Special Issue. 3-D acoustics and oceanographic effects were of particular interest. 2) Begin 2016 experimental planning, both on an individual basis, and in conjunction with the whole ocean acoustics community.
author2 WOODS HOLE OCEANOGRAPHIC INSTITUTION MA
format Text
author Lynch, James F
author_facet Lynch, James F
author_sort Lynch, James F
title SW06 Data Analysis, Slope-Canyon Experiment Planning, and Long-Range Sound Propagation with Applications to the Arctic
title_short SW06 Data Analysis, Slope-Canyon Experiment Planning, and Long-Range Sound Propagation with Applications to the Arctic
title_full SW06 Data Analysis, Slope-Canyon Experiment Planning, and Long-Range Sound Propagation with Applications to the Arctic
title_fullStr SW06 Data Analysis, Slope-Canyon Experiment Planning, and Long-Range Sound Propagation with Applications to the Arctic
title_full_unstemmed SW06 Data Analysis, Slope-Canyon Experiment Planning, and Long-Range Sound Propagation with Applications to the Arctic
title_sort sw06 data analysis, slope-canyon experiment planning, and long-range sound propagation with applications to the arctic
publishDate 2011
url http://www.dtic.mil/docs/citations/ADA571750
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA571750
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source DTIC
op_relation http://www.dtic.mil/docs/citations/ADA571750
op_rights Approved for public release; distribution is unlimited.
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