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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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. |
_version_ |
1766313215557369856 |