Arctic Under-Ice Roughness.

Under-ice profile records obtained in the Arctic Ocean during the winter 1960 cruise of the USS SARGO and the 1960 and 1962 summer cruises of the USS SEADRAGON have been digitized and the Root-Mean-Square (RMS) depths have been computed (The RMS ice depth is a valuable parameter for Arctic acoustic...

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Bibliographic Details
Main Authors: LeSchack,Leonard A, Chang,David C
Other Authors: DEVELOPMENT AND RESOURCES TRANSPORTATION CO SILVER SPRING MD
Format: Text
Language:English
Published: 1977
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA048690
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA048690
id ftdtic:ADA048690
record_format openpolar
spelling ftdtic:ADA048690 2023-05-15T14:42:01+02:00 Arctic Under-Ice Roughness. LeSchack,Leonard A Chang,David C DEVELOPMENT AND RESOURCES TRANSPORTATION CO SILVER SPRING MD 1977-12 text/html http://www.dtic.mil/docs/citations/ADA048690 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA048690 en eng http://www.dtic.mil/docs/citations/ADA048690 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost Underwater and Marine Navigation and Guidance Acoustics *UNDERWATER ACOUSTICS *UNDERWATER NAVIGATION *SEA ICE *ARCTIC OCEAN THICKNESS SEASONAL VARIATIONS SUBMARINES ROUGHNESS SONAR TRANSDUCERS SONAR SIGNALS SHALLOW DEPTH Under ice roughness WUNR307374 Most Project-2 Text 1977 ftdtic 2016-02-20T14:51:31Z Under-ice profile records obtained in the Arctic Ocean during the winter 1960 cruise of the USS SARGO and the 1960 and 1962 summer cruises of the USS SEADRAGON have been digitized and the Root-Mean-Square (RMS) depths have been computed (The RMS ice depth is a valuable parameter for Arctic acoustic studies as well as a good indicator of under-ice roughness). Thirteen representative profile segments varying in length from 50-250 miles and taken from the three cruises have been statistically analyzed. This analysis suggests that during the 1960-62 period under-ice roughness varies from place to place during the same period but at a given location does not vary over time. Histograms of ice depths observed across the Arctic Ocean during the above three cruises have been plotted. From these plots it is observed that there is, for this period, 15% open water in the summer and 2% during the winter. Additionally, it is noted that the amount of ice found in each thickness class varies only a few percent between winter and the following summers. (Author) Text Arctic Arctic Ocean Ice permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Snow
Ice and Permafrost
Underwater and Marine Navigation and Guidance
Acoustics
*UNDERWATER ACOUSTICS
*UNDERWATER NAVIGATION
*SEA ICE
*ARCTIC OCEAN
THICKNESS
SEASONAL VARIATIONS
SUBMARINES
ROUGHNESS
SONAR TRANSDUCERS
SONAR SIGNALS
SHALLOW DEPTH
Under ice roughness
WUNR307374
Most Project-2
spellingShingle Snow
Ice and Permafrost
Underwater and Marine Navigation and Guidance
Acoustics
*UNDERWATER ACOUSTICS
*UNDERWATER NAVIGATION
*SEA ICE
*ARCTIC OCEAN
THICKNESS
SEASONAL VARIATIONS
SUBMARINES
ROUGHNESS
SONAR TRANSDUCERS
SONAR SIGNALS
SHALLOW DEPTH
Under ice roughness
WUNR307374
Most Project-2
LeSchack,Leonard A
Chang,David C
Arctic Under-Ice Roughness.
topic_facet Snow
Ice and Permafrost
Underwater and Marine Navigation and Guidance
Acoustics
*UNDERWATER ACOUSTICS
*UNDERWATER NAVIGATION
*SEA ICE
*ARCTIC OCEAN
THICKNESS
SEASONAL VARIATIONS
SUBMARINES
ROUGHNESS
SONAR TRANSDUCERS
SONAR SIGNALS
SHALLOW DEPTH
Under ice roughness
WUNR307374
Most Project-2
description Under-ice profile records obtained in the Arctic Ocean during the winter 1960 cruise of the USS SARGO and the 1960 and 1962 summer cruises of the USS SEADRAGON have been digitized and the Root-Mean-Square (RMS) depths have been computed (The RMS ice depth is a valuable parameter for Arctic acoustic studies as well as a good indicator of under-ice roughness). Thirteen representative profile segments varying in length from 50-250 miles and taken from the three cruises have been statistically analyzed. This analysis suggests that during the 1960-62 period under-ice roughness varies from place to place during the same period but at a given location does not vary over time. Histograms of ice depths observed across the Arctic Ocean during the above three cruises have been plotted. From these plots it is observed that there is, for this period, 15% open water in the summer and 2% during the winter. Additionally, it is noted that the amount of ice found in each thickness class varies only a few percent between winter and the following summers. (Author)
author2 DEVELOPMENT AND RESOURCES TRANSPORTATION CO SILVER SPRING MD
format Text
author LeSchack,Leonard A
Chang,David C
author_facet LeSchack,Leonard A
Chang,David C
author_sort LeSchack,Leonard A
title Arctic Under-Ice Roughness.
title_short Arctic Under-Ice Roughness.
title_full Arctic Under-Ice Roughness.
title_fullStr Arctic Under-Ice Roughness.
title_full_unstemmed Arctic Under-Ice Roughness.
title_sort arctic under-ice roughness.
publishDate 1977
url http://www.dtic.mil/docs/citations/ADA048690
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA048690
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Ice
permafrost
Sea ice
genre_facet Arctic
Arctic Ocean
Ice
permafrost
Sea ice
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA048690
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766313696230899712