Ice Statistics and Acoustic Scattering in the Arctic Basin.

Acoustic propagation in the Arctic is intimately related to the structure of surface pack ice. In this paper, reflection loss and transmission loss are calculated based upon statistical models of ice roughness. Statistical models of ice ridges are introduced and techniques for estimating the roughne...

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Bibliographic Details
Main Author: Greene,R R
Other Authors: SCIENCE APPLICATIONS INTERNATIONAL CORP MCLEAN VA
Format: Text
Language:English
Published: 1984
Subjects:
ICE
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA150141
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA150141
id ftdtic:ADA150141
record_format openpolar
spelling ftdtic:ADA150141 2023-05-15T14:29:12+02:00 Ice Statistics and Acoustic Scattering in the Arctic Basin. Greene,R R SCIENCE APPLICATIONS INTERNATIONAL CORP MCLEAN VA 1984-10-01 text/html http://www.dtic.mil/docs/citations/ADA150141 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA150141 en eng http://www.dtic.mil/docs/citations/ADA150141 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost Acoustics *TRANSMISSION LOSS SURFACE ROUGHNESS ICE SOUND TRANSMISSION PARABOLAS STATISTICAL ANALYSIS EQUATIONS ACOUSTIC SCATTERING ARCTIC REGIONS HIGH ANGLES ACOUSTIC REFLECTION RIDGES ARCTIC OCEAN PACK ICE UNDERICE ARCHAPE(Arctic High Angle Parabolic Equations) Parabolic equations Text 1984 ftdtic 2016-02-20T23:45:54Z Acoustic propagation in the Arctic is intimately related to the structure of surface pack ice. In this paper, reflection loss and transmission loss are calculated based upon statistical models of ice roughness. Statistical models of ice ridges are introduced and techniques for estimating the roughness spectrum of ridged surfaces are developed. Next, a model for estimating the mean reflection loss is introduced. The reflection loss formulas are based on the statistical models for roughness. Transmission loss calculations using High-Angle parabolic equation (ARCHAPE) in a simulated Arctic environment are compared with data. The results demonstrate that rough surface scattering from random-depth ice keel structures can account for the observed rate of transmission loss in the Arctic. Keywords include: Acoustic Scattering, and Propagation loss. Text Arctic Basin Arctic Arctic Ocean Ice permafrost 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
Acoustics
*TRANSMISSION LOSS
SURFACE ROUGHNESS
ICE
SOUND TRANSMISSION
PARABOLAS
STATISTICAL ANALYSIS
EQUATIONS
ACOUSTIC SCATTERING
ARCTIC REGIONS
HIGH ANGLES
ACOUSTIC REFLECTION
RIDGES
ARCTIC OCEAN
PACK ICE
UNDERICE
ARCHAPE(Arctic High Angle Parabolic Equations)
Parabolic equations
spellingShingle Snow
Ice and Permafrost
Acoustics
*TRANSMISSION LOSS
SURFACE ROUGHNESS
ICE
SOUND TRANSMISSION
PARABOLAS
STATISTICAL ANALYSIS
EQUATIONS
ACOUSTIC SCATTERING
ARCTIC REGIONS
HIGH ANGLES
ACOUSTIC REFLECTION
RIDGES
ARCTIC OCEAN
PACK ICE
UNDERICE
ARCHAPE(Arctic High Angle Parabolic Equations)
Parabolic equations
Greene,R R
Ice Statistics and Acoustic Scattering in the Arctic Basin.
topic_facet Snow
Ice and Permafrost
Acoustics
*TRANSMISSION LOSS
SURFACE ROUGHNESS
ICE
SOUND TRANSMISSION
PARABOLAS
STATISTICAL ANALYSIS
EQUATIONS
ACOUSTIC SCATTERING
ARCTIC REGIONS
HIGH ANGLES
ACOUSTIC REFLECTION
RIDGES
ARCTIC OCEAN
PACK ICE
UNDERICE
ARCHAPE(Arctic High Angle Parabolic Equations)
Parabolic equations
description Acoustic propagation in the Arctic is intimately related to the structure of surface pack ice. In this paper, reflection loss and transmission loss are calculated based upon statistical models of ice roughness. Statistical models of ice ridges are introduced and techniques for estimating the roughness spectrum of ridged surfaces are developed. Next, a model for estimating the mean reflection loss is introduced. The reflection loss formulas are based on the statistical models for roughness. Transmission loss calculations using High-Angle parabolic equation (ARCHAPE) in a simulated Arctic environment are compared with data. The results demonstrate that rough surface scattering from random-depth ice keel structures can account for the observed rate of transmission loss in the Arctic. Keywords include: Acoustic Scattering, and Propagation loss.
author2 SCIENCE APPLICATIONS INTERNATIONAL CORP MCLEAN VA
format Text
author Greene,R R
author_facet Greene,R R
author_sort Greene,R R
title Ice Statistics and Acoustic Scattering in the Arctic Basin.
title_short Ice Statistics and Acoustic Scattering in the Arctic Basin.
title_full Ice Statistics and Acoustic Scattering in the Arctic Basin.
title_fullStr Ice Statistics and Acoustic Scattering in the Arctic Basin.
title_full_unstemmed Ice Statistics and Acoustic Scattering in the Arctic Basin.
title_sort ice statistics and acoustic scattering in the arctic basin.
publishDate 1984
url http://www.dtic.mil/docs/citations/ADA150141
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA150141
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic Basin
Arctic
Arctic Ocean
Ice
permafrost
genre_facet Arctic Basin
Arctic
Arctic Ocean
Ice
permafrost
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA150141
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766303271537868800