Depth and Seasonal Dependence of Ambient Sea Noise Near the Marginal Ice Zone of the Greenland Sea

Omnidirectional data from seasonal and short-term (several days), depth-dependent ambient sea-noise measurements in the 20-to-600-Hz band near the marginal ice zone were recorded in the deepwater basin of the Greenland Sea. Two bottom-anchored, self-supporting buoys, one of which recorded acoustic d...

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Bibliographic Details
Main Author: McGrath, James R
Other Authors: NAVAL RESEARCH LAB WASHINGTON DC
Format: Text
Language:English
Published: 1976
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA025212
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA025212
id ftdtic:ADA025212
record_format openpolar
spelling ftdtic:ADA025212 2023-05-15T15:11:31+02:00 Depth and Seasonal Dependence of Ambient Sea Noise Near the Marginal Ice Zone of the Greenland Sea McGrath, James R NAVAL RESEARCH LAB WASHINGTON DC 1976-04-01 text/html http://www.dtic.mil/docs/citations/ADA025212 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA025212 en eng http://www.dtic.mil/docs/citations/ADA025212 Approved for public release; distribution is unlimited. DTIC AND NTIS Snow Ice and Permafrost Acoustics *AMBIENT NOISE *SEA ICE *UNDERWATER SOUND ACOUSTIC DATA BOUNDARIES DEEP WATER DEPTH EXTREMELY LOW FREQUENCY GREENLAND SEA HYDROPHONES INTENSITY OMNIDIRECTIONAL OPEN WATER SEASONAL VARIATIONS SOURCES WIND DIRECTION WIND VELOCITY Marginal ice zone Ice floes Most Project-2 Text 1976 ftdtic 2016-02-24T11:27:52Z Omnidirectional data from seasonal and short-term (several days), depth-dependent ambient sea-noise measurements in the 20-to-600-Hz band near the marginal ice zone were recorded in the deepwater basin of the Greenland Sea. Two bottom-anchored, self-supporting buoys, one of which recorded acoustic data for 9 months, were used. The first experiment, conducted between Aug 1972 and July 1973, recorded 1-min samples of sea noise every 4 h from an omnidirectional hydrophone 306 m below the surface. During this time, the ice edge moved over the recording site, providing evidence that the iceline acts as a noise source, raising levels above both open-ocean and icefield values. Seasonal conditions favor the lowest ambient noise levels during midwinter (Jan) and early summer (June), while the highest levels occur during early spring (March) and early fall (Nov). Evidence indicates that the maximum ambient noise levels near the marginal ice zone are 12 to 16 dB higher than the maximum Arctic Ocean values under contiguous ice cover. The second experiment, conducted over a 5-day period, recorded ambient noise at depths of 241, 1,232, 1,537, and 2,375 m. Results indicate that ambient noise levels near the ice edge within the water column depend on speed and direction of wind. Text Arctic Arctic Ocean Greenland Greenland Sea Ice permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean Greenland Midwinter ENVELOPE(139.931,139.931,-66.690,-66.690)
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Snow
Ice and Permafrost
Acoustics
*AMBIENT NOISE
*SEA ICE
*UNDERWATER SOUND
ACOUSTIC DATA
BOUNDARIES
DEEP WATER
DEPTH
EXTREMELY LOW FREQUENCY
GREENLAND SEA
HYDROPHONES
INTENSITY
OMNIDIRECTIONAL
OPEN WATER
SEASONAL VARIATIONS
SOURCES
WIND DIRECTION
WIND VELOCITY
Marginal ice zone
Ice floes
Most Project-2
spellingShingle Snow
Ice and Permafrost
Acoustics
*AMBIENT NOISE
*SEA ICE
*UNDERWATER SOUND
ACOUSTIC DATA
BOUNDARIES
DEEP WATER
DEPTH
EXTREMELY LOW FREQUENCY
GREENLAND SEA
HYDROPHONES
INTENSITY
OMNIDIRECTIONAL
OPEN WATER
SEASONAL VARIATIONS
SOURCES
WIND DIRECTION
WIND VELOCITY
Marginal ice zone
Ice floes
Most Project-2
McGrath, James R
Depth and Seasonal Dependence of Ambient Sea Noise Near the Marginal Ice Zone of the Greenland Sea
topic_facet Snow
Ice and Permafrost
Acoustics
*AMBIENT NOISE
*SEA ICE
*UNDERWATER SOUND
ACOUSTIC DATA
BOUNDARIES
DEEP WATER
DEPTH
EXTREMELY LOW FREQUENCY
GREENLAND SEA
HYDROPHONES
INTENSITY
OMNIDIRECTIONAL
OPEN WATER
SEASONAL VARIATIONS
SOURCES
WIND DIRECTION
WIND VELOCITY
Marginal ice zone
Ice floes
Most Project-2
description Omnidirectional data from seasonal and short-term (several days), depth-dependent ambient sea-noise measurements in the 20-to-600-Hz band near the marginal ice zone were recorded in the deepwater basin of the Greenland Sea. Two bottom-anchored, self-supporting buoys, one of which recorded acoustic data for 9 months, were used. The first experiment, conducted between Aug 1972 and July 1973, recorded 1-min samples of sea noise every 4 h from an omnidirectional hydrophone 306 m below the surface. During this time, the ice edge moved over the recording site, providing evidence that the iceline acts as a noise source, raising levels above both open-ocean and icefield values. Seasonal conditions favor the lowest ambient noise levels during midwinter (Jan) and early summer (June), while the highest levels occur during early spring (March) and early fall (Nov). Evidence indicates that the maximum ambient noise levels near the marginal ice zone are 12 to 16 dB higher than the maximum Arctic Ocean values under contiguous ice cover. The second experiment, conducted over a 5-day period, recorded ambient noise at depths of 241, 1,232, 1,537, and 2,375 m. Results indicate that ambient noise levels near the ice edge within the water column depend on speed and direction of wind.
author2 NAVAL RESEARCH LAB WASHINGTON DC
format Text
author McGrath, James R
author_facet McGrath, James R
author_sort McGrath, James R
title Depth and Seasonal Dependence of Ambient Sea Noise Near the Marginal Ice Zone of the Greenland Sea
title_short Depth and Seasonal Dependence of Ambient Sea Noise Near the Marginal Ice Zone of the Greenland Sea
title_full Depth and Seasonal Dependence of Ambient Sea Noise Near the Marginal Ice Zone of the Greenland Sea
title_fullStr Depth and Seasonal Dependence of Ambient Sea Noise Near the Marginal Ice Zone of the Greenland Sea
title_full_unstemmed Depth and Seasonal Dependence of Ambient Sea Noise Near the Marginal Ice Zone of the Greenland Sea
title_sort depth and seasonal dependence of ambient sea noise near the marginal ice zone of the greenland sea
publishDate 1976
url http://www.dtic.mil/docs/citations/ADA025212
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA025212
long_lat ENVELOPE(139.931,139.931,-66.690,-66.690)
geographic Arctic
Arctic Ocean
Greenland
Midwinter
geographic_facet Arctic
Arctic Ocean
Greenland
Midwinter
genre Arctic
Arctic Ocean
Greenland
Greenland Sea
Ice
permafrost
Sea ice
genre_facet Arctic
Arctic Ocean
Greenland
Greenland Sea
Ice
permafrost
Sea ice
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA025212
op_rights Approved for public release; distribution is unlimited.
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