Thin-ice Arctic Acoustic Window (THAAW)

The Arctic Ocean is currently undergoing dramatic changes, including reductions in the extent and thickness of the ice cover and extensive warming of the intermediate layers. The multiyear ice is melting. Ice keels are getting smaller. With more open water, the internal wave energy level and therefo...

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Main Authors: Worcester, Peter F, Cornuelle, Bruce D, Dzieciuch, Matthew A, Munk, Walter H
Other Authors: SCRIPPS INSTITUTION OF OCEANOGRAPHY LA JOLLA CA
Format: Text
Language:English
Published: 2014
Subjects:
ICE
Online Access:http://www.dtic.mil/docs/citations/ADA618125
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA618125
id ftdtic:ADA618125
record_format openpolar
spelling ftdtic:ADA618125 2023-05-15T14:33:48+02:00 Thin-ice Arctic Acoustic Window (THAAW) Worcester, Peter F Cornuelle, Bruce D Dzieciuch, Matthew A Munk, Walter H SCRIPPS INSTITUTION OF OCEANOGRAPHY LA JOLLA CA 2014-09-30 text/html http://www.dtic.mil/docs/citations/ADA618125 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA618125 en eng http://www.dtic.mil/docs/citations/ADA618125 Approved for public release; distribution is unlimited. DTIC Acoustics *ACOUSTIC WINDOWS AMBIENT NOISE ARCTIC OCEAN ICE LOW FREQUENCY OPEN WATER SIGNAL PROCESSING THAAW(THIN-ICE ARCTIC ACOUSTIC WINDOW) Text 2014 ftdtic 2016-02-24T18:03:38Z The Arctic Ocean is currently undergoing dramatic changes, including reductions in the extent and thickness of the ice cover and extensive warming of the intermediate layers. The multiyear ice is melting. Ice keels are getting smaller. With more open water, the internal wave energy level and therefore acoustic volume scattering are likely increasing, at least during summer. What was learned about acoustic propagation and ambient noise in the Arctic during the Cold War is now obsolete. The long-term objectives of this research program are to understand the effects of changing Arctic conditions on low-frequency, deep-water propagation and on the low-frequency ambient noise field. The goal is to determine the fundamental limits to signal processing in the Arctic imposed by ocean and ice processes. The hope is that these first few new steps will lead to a larger, permanent acoustic monitoring, communications, and navigation network in the Arctic Ocean (Mikhalevsky et al., 2014). This research effort was funded as an expansion of ONR Grant N00014-12-1-0226, entitled North Pacific Acoustic Laboratory: Deep Water Acoustic Propagation in the Philippine Sea. This annual report is in addition to the annual report for ONR Grant N00014-12-1-0226 that describes the research effort in the Philippine Sea. Text Arctic Arctic Ocean Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean Pacific
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Acoustics
*ACOUSTIC WINDOWS
AMBIENT NOISE
ARCTIC OCEAN
ICE
LOW FREQUENCY
OPEN WATER
SIGNAL PROCESSING
THAAW(THIN-ICE ARCTIC ACOUSTIC WINDOW)
spellingShingle Acoustics
*ACOUSTIC WINDOWS
AMBIENT NOISE
ARCTIC OCEAN
ICE
LOW FREQUENCY
OPEN WATER
SIGNAL PROCESSING
THAAW(THIN-ICE ARCTIC ACOUSTIC WINDOW)
Worcester, Peter F
Cornuelle, Bruce D
Dzieciuch, Matthew A
Munk, Walter H
Thin-ice Arctic Acoustic Window (THAAW)
topic_facet Acoustics
*ACOUSTIC WINDOWS
AMBIENT NOISE
ARCTIC OCEAN
ICE
LOW FREQUENCY
OPEN WATER
SIGNAL PROCESSING
THAAW(THIN-ICE ARCTIC ACOUSTIC WINDOW)
description The Arctic Ocean is currently undergoing dramatic changes, including reductions in the extent and thickness of the ice cover and extensive warming of the intermediate layers. The multiyear ice is melting. Ice keels are getting smaller. With more open water, the internal wave energy level and therefore acoustic volume scattering are likely increasing, at least during summer. What was learned about acoustic propagation and ambient noise in the Arctic during the Cold War is now obsolete. The long-term objectives of this research program are to understand the effects of changing Arctic conditions on low-frequency, deep-water propagation and on the low-frequency ambient noise field. The goal is to determine the fundamental limits to signal processing in the Arctic imposed by ocean and ice processes. The hope is that these first few new steps will lead to a larger, permanent acoustic monitoring, communications, and navigation network in the Arctic Ocean (Mikhalevsky et al., 2014). This research effort was funded as an expansion of ONR Grant N00014-12-1-0226, entitled North Pacific Acoustic Laboratory: Deep Water Acoustic Propagation in the Philippine Sea. This annual report is in addition to the annual report for ONR Grant N00014-12-1-0226 that describes the research effort in the Philippine Sea.
author2 SCRIPPS INSTITUTION OF OCEANOGRAPHY LA JOLLA CA
format Text
author Worcester, Peter F
Cornuelle, Bruce D
Dzieciuch, Matthew A
Munk, Walter H
author_facet Worcester, Peter F
Cornuelle, Bruce D
Dzieciuch, Matthew A
Munk, Walter H
author_sort Worcester, Peter F
title Thin-ice Arctic Acoustic Window (THAAW)
title_short Thin-ice Arctic Acoustic Window (THAAW)
title_full Thin-ice Arctic Acoustic Window (THAAW)
title_fullStr Thin-ice Arctic Acoustic Window (THAAW)
title_full_unstemmed Thin-ice Arctic Acoustic Window (THAAW)
title_sort thin-ice arctic acoustic window (thaaw)
publishDate 2014
url http://www.dtic.mil/docs/citations/ADA618125
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA618125
geographic Arctic
Arctic Ocean
Pacific
geographic_facet Arctic
Arctic Ocean
Pacific
genre Arctic
Arctic Ocean
genre_facet Arctic
Arctic Ocean
op_source DTIC
op_relation http://www.dtic.mil/docs/citations/ADA618125
op_rights Approved for public release; distribution is unlimited.
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