Low-Frequency Acoustic Propagation Loss in the Arctic Ocean: Results of the Arctic Climate Observations using Underwater Sound Experiment

Acoustic data from the Arctic Climate Observations using Underwater Sound (ACOUS) experiment are analyzed to determine the correlation between acoustic propagation loss and the seasonal variability of sea ice thickness. The objective of this research is to provide long-term synoptic monitoring of se...

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Main Authors: Gavrilov, Alexander N., Mikhalevsky, Peter N.
Other Authors: SCIENCE APPLICATIONS INTERNATIONAL CORPMCLEAN VA
Format: Text
Language:English
Published: 2004
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA433378
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA433378
id ftdtic:ADA433378
record_format openpolar
spelling ftdtic:ADA433378 2023-05-15T14:41:27+02:00 Low-Frequency Acoustic Propagation Loss in the Arctic Ocean: Results of the Arctic Climate Observations using Underwater Sound Experiment Gavrilov, Alexander N. Mikhalevsky, Peter N. SCIENCE APPLICATIONS INTERNATIONAL CORPMCLEAN VA 2004-03-05 text/html http://www.dtic.mil/docs/citations/ADA433378 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA433378 en eng http://www.dtic.mil/docs/citations/ADA433378 Approved for public release; distribution is unlimited., Availability: This document is not available from DTIC in microfiche. DTIC AND NTIS Snow Ice and Permafrost Acoustics *ACOUSTIC DATA *SEA ICE *ARCTIC OCEAN MATHEMATICAL MODELS COUPLING(INTERACTION) PROPAGATION THICKNESS PARAMETERS ARRAYS SEASONAL VARIATIONS MATHEMATICAL PREDICTION VERTICAL ORIENTATION SIGNALS REMOTE DETECTORS SOUND TRANSMISSION CLIMATE TOMOGRAPHY ACOUSTIC VELOCITY LOW FREQUENCY UNDERWATER SOUND TRANSMISSION LOSS ARCTIC REGIONS NOISE(SOUND) ACOUSTIC DETECTORS FRANZ JOSEF LAND ACOUS(ARCTIC OBSERVATIONS USING UNDERWATER SOUND) Text 2004 ftdtic 2016-02-21T10:36:12Z Acoustic data from the Arctic Climate Observations using Underwater Sound (ACOUS) experiment are analyzed to determine the correlation between acoustic propagation loss and the seasonal variability of sea ice thickness. The objective of this research is to provide long-term synoptic monitoring of sea ice thickness, an important global climate variable, using acoustic remote sensing. As part of the ACOUS program an autonomous acoustic source deployed northwest of Franz Josef Land transmitted tomographic signals at 20.5 Hz once every four days from October 1998 until December 1999. These signals were received on a vertical array in the Lincoln Sea 1250 km away. Two of the signals transmitted in April 1999 were received on a vertical array at ice camp APLIS in the Chukehi Sea north of Point Barrow, Alaska, at a distance of approximately 2720 kin from the source. Temporal variations of the modal propagation loss are examined. The influence of ice parameters, variations of the sound speed profile, and mode- coupling effects on the propagation losses of individual modes is studied. The experimental results are compared to the results of the earlier experiments and the theoretical prediction using numerical modeling. The original document contains color images. Text Arctic Arctic Ocean Barrow Franz Josef Land Ice Lincoln Sea permafrost Point Barrow Sea ice Alaska Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean Franz Josef Land ENVELOPE(55.000,55.000,81.000,81.000)
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Snow
Ice and Permafrost
Acoustics
*ACOUSTIC DATA
*SEA ICE
*ARCTIC OCEAN
MATHEMATICAL MODELS
COUPLING(INTERACTION)
PROPAGATION
THICKNESS
PARAMETERS
ARRAYS
SEASONAL VARIATIONS
MATHEMATICAL PREDICTION
VERTICAL ORIENTATION
SIGNALS
REMOTE DETECTORS
SOUND TRANSMISSION
CLIMATE
TOMOGRAPHY
ACOUSTIC VELOCITY
LOW FREQUENCY
UNDERWATER SOUND
TRANSMISSION LOSS
ARCTIC REGIONS
NOISE(SOUND)
ACOUSTIC DETECTORS
FRANZ JOSEF LAND
ACOUS(ARCTIC OBSERVATIONS USING UNDERWATER SOUND)
spellingShingle Snow
Ice and Permafrost
Acoustics
*ACOUSTIC DATA
*SEA ICE
*ARCTIC OCEAN
MATHEMATICAL MODELS
COUPLING(INTERACTION)
PROPAGATION
THICKNESS
PARAMETERS
ARRAYS
SEASONAL VARIATIONS
MATHEMATICAL PREDICTION
VERTICAL ORIENTATION
SIGNALS
REMOTE DETECTORS
SOUND TRANSMISSION
CLIMATE
TOMOGRAPHY
ACOUSTIC VELOCITY
LOW FREQUENCY
UNDERWATER SOUND
TRANSMISSION LOSS
ARCTIC REGIONS
NOISE(SOUND)
ACOUSTIC DETECTORS
FRANZ JOSEF LAND
ACOUS(ARCTIC OBSERVATIONS USING UNDERWATER SOUND)
Gavrilov, Alexander N.
Mikhalevsky, Peter N.
Low-Frequency Acoustic Propagation Loss in the Arctic Ocean: Results of the Arctic Climate Observations using Underwater Sound Experiment
topic_facet Snow
Ice and Permafrost
Acoustics
*ACOUSTIC DATA
*SEA ICE
*ARCTIC OCEAN
MATHEMATICAL MODELS
COUPLING(INTERACTION)
PROPAGATION
THICKNESS
PARAMETERS
ARRAYS
SEASONAL VARIATIONS
MATHEMATICAL PREDICTION
VERTICAL ORIENTATION
SIGNALS
REMOTE DETECTORS
SOUND TRANSMISSION
CLIMATE
TOMOGRAPHY
ACOUSTIC VELOCITY
LOW FREQUENCY
UNDERWATER SOUND
TRANSMISSION LOSS
ARCTIC REGIONS
NOISE(SOUND)
ACOUSTIC DETECTORS
FRANZ JOSEF LAND
ACOUS(ARCTIC OBSERVATIONS USING UNDERWATER SOUND)
description Acoustic data from the Arctic Climate Observations using Underwater Sound (ACOUS) experiment are analyzed to determine the correlation between acoustic propagation loss and the seasonal variability of sea ice thickness. The objective of this research is to provide long-term synoptic monitoring of sea ice thickness, an important global climate variable, using acoustic remote sensing. As part of the ACOUS program an autonomous acoustic source deployed northwest of Franz Josef Land transmitted tomographic signals at 20.5 Hz once every four days from October 1998 until December 1999. These signals were received on a vertical array in the Lincoln Sea 1250 km away. Two of the signals transmitted in April 1999 were received on a vertical array at ice camp APLIS in the Chukehi Sea north of Point Barrow, Alaska, at a distance of approximately 2720 kin from the source. Temporal variations of the modal propagation loss are examined. The influence of ice parameters, variations of the sound speed profile, and mode- coupling effects on the propagation losses of individual modes is studied. The experimental results are compared to the results of the earlier experiments and the theoretical prediction using numerical modeling. The original document contains color images.
author2 SCIENCE APPLICATIONS INTERNATIONAL CORPMCLEAN VA
format Text
author Gavrilov, Alexander N.
Mikhalevsky, Peter N.
author_facet Gavrilov, Alexander N.
Mikhalevsky, Peter N.
author_sort Gavrilov, Alexander N.
title Low-Frequency Acoustic Propagation Loss in the Arctic Ocean: Results of the Arctic Climate Observations using Underwater Sound Experiment
title_short Low-Frequency Acoustic Propagation Loss in the Arctic Ocean: Results of the Arctic Climate Observations using Underwater Sound Experiment
title_full Low-Frequency Acoustic Propagation Loss in the Arctic Ocean: Results of the Arctic Climate Observations using Underwater Sound Experiment
title_fullStr Low-Frequency Acoustic Propagation Loss in the Arctic Ocean: Results of the Arctic Climate Observations using Underwater Sound Experiment
title_full_unstemmed Low-Frequency Acoustic Propagation Loss in the Arctic Ocean: Results of the Arctic Climate Observations using Underwater Sound Experiment
title_sort low-frequency acoustic propagation loss in the arctic ocean: results of the arctic climate observations using underwater sound experiment
publishDate 2004
url http://www.dtic.mil/docs/citations/ADA433378
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA433378
long_lat ENVELOPE(55.000,55.000,81.000,81.000)
geographic Arctic
Arctic Ocean
Franz Josef Land
geographic_facet Arctic
Arctic Ocean
Franz Josef Land
genre Arctic
Arctic Ocean
Barrow
Franz Josef Land
Ice
Lincoln Sea
permafrost
Point Barrow
Sea ice
Alaska
genre_facet Arctic
Arctic Ocean
Barrow
Franz Josef Land
Ice
Lincoln Sea
permafrost
Point Barrow
Sea ice
Alaska
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA433378
op_rights Approved for public release; distribution is unlimited., Availability: This document is not available from DTIC in microfiche.
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