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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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 |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
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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. |
_version_ |
1766337326359773184 |