Acoustic Scattering Kernels from Arctic Sea Ice.

A new algorithm for computing scattering kernels from Artic ice keels is described. The basic equations are adapted from Burke and Twersky (1966) but the algorithm does not involve approximations in the limits of low or high frequencies, and is therefore more accurate. Calculations over a range of f...

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Bibliographic Details
Main Author: Rubenstein,David
Other Authors: SCIENCE APPLICATIONS INTERNATIONAL CORP MCLEAN VA
Format: Text
Language:English
Published: 1986
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA174235
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA174235
id ftdtic:ADA174235
record_format openpolar
spelling ftdtic:ADA174235 2023-05-15T14:52:50+02:00 Acoustic Scattering Kernels from Arctic Sea Ice. Rubenstein,David SCIENCE APPLICATIONS INTERNATIONAL CORP MCLEAN VA 1986-10 text/html http://www.dtic.mil/docs/citations/ADA174235 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA174235 en eng http://www.dtic.mil/docs/citations/ADA174235 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost Acoustics *ACOUSTIC SCATTERING *SEA ICE ALGORITHMS ANGLES SURFACE ROUGHNESS TOPOGRAPHY KERNEL FUNCTIONS INCOHERENT SCATTERING UNDERWATER ACOUSTICS TRANSMISSION LOSS ARCTIC REGIONS ACOUSTIC REFLECTION RIDGES GRAZING ACOUSTIC CHANNELS UNDERICE Ice keels Grazing angles Scattering loss Underice surfaces Mathieu function Text 1986 ftdtic 2016-02-21T02:42:13Z A new algorithm for computing scattering kernels from Artic ice keels is described. The basic equations are adapted from Burke and Twersky (1966) but the algorithm does not involve approximations in the limits of low or high frequencies, and is therefore more accurate. Calculations over a range of frequencies and grazing angles are presented. An important result is obtained. At high frequencies (greater than 200 hz) a significant component of the incoherent scattered energy is directed into shallow propagation angles (less than 15 degrees). This component must be accounted for in estimates of scattering loss. Text Arctic Ice permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database Arctic Mathieu ENVELOPE(136.814,136.814,-66.331,-66.331)
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 SCATTERING
*SEA ICE
ALGORITHMS
ANGLES
SURFACE ROUGHNESS
TOPOGRAPHY
KERNEL FUNCTIONS
INCOHERENT SCATTERING
UNDERWATER ACOUSTICS
TRANSMISSION LOSS
ARCTIC REGIONS
ACOUSTIC REFLECTION
RIDGES
GRAZING
ACOUSTIC CHANNELS
UNDERICE
Ice keels
Grazing angles
Scattering loss
Underice surfaces
Mathieu function
spellingShingle Snow
Ice and Permafrost
Acoustics
*ACOUSTIC SCATTERING
*SEA ICE
ALGORITHMS
ANGLES
SURFACE ROUGHNESS
TOPOGRAPHY
KERNEL FUNCTIONS
INCOHERENT SCATTERING
UNDERWATER ACOUSTICS
TRANSMISSION LOSS
ARCTIC REGIONS
ACOUSTIC REFLECTION
RIDGES
GRAZING
ACOUSTIC CHANNELS
UNDERICE
Ice keels
Grazing angles
Scattering loss
Underice surfaces
Mathieu function
Rubenstein,David
Acoustic Scattering Kernels from Arctic Sea Ice.
topic_facet Snow
Ice and Permafrost
Acoustics
*ACOUSTIC SCATTERING
*SEA ICE
ALGORITHMS
ANGLES
SURFACE ROUGHNESS
TOPOGRAPHY
KERNEL FUNCTIONS
INCOHERENT SCATTERING
UNDERWATER ACOUSTICS
TRANSMISSION LOSS
ARCTIC REGIONS
ACOUSTIC REFLECTION
RIDGES
GRAZING
ACOUSTIC CHANNELS
UNDERICE
Ice keels
Grazing angles
Scattering loss
Underice surfaces
Mathieu function
description A new algorithm for computing scattering kernels from Artic ice keels is described. The basic equations are adapted from Burke and Twersky (1966) but the algorithm does not involve approximations in the limits of low or high frequencies, and is therefore more accurate. Calculations over a range of frequencies and grazing angles are presented. An important result is obtained. At high frequencies (greater than 200 hz) a significant component of the incoherent scattered energy is directed into shallow propagation angles (less than 15 degrees). This component must be accounted for in estimates of scattering loss.
author2 SCIENCE APPLICATIONS INTERNATIONAL CORP MCLEAN VA
format Text
author Rubenstein,David
author_facet Rubenstein,David
author_sort Rubenstein,David
title Acoustic Scattering Kernels from Arctic Sea Ice.
title_short Acoustic Scattering Kernels from Arctic Sea Ice.
title_full Acoustic Scattering Kernels from Arctic Sea Ice.
title_fullStr Acoustic Scattering Kernels from Arctic Sea Ice.
title_full_unstemmed Acoustic Scattering Kernels from Arctic Sea Ice.
title_sort acoustic scattering kernels from arctic sea ice.
publishDate 1986
url http://www.dtic.mil/docs/citations/ADA174235
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA174235
long_lat ENVELOPE(136.814,136.814,-66.331,-66.331)
geographic Arctic
Mathieu
geographic_facet Arctic
Mathieu
genre Arctic
Ice
permafrost
Sea ice
genre_facet Arctic
Ice
permafrost
Sea ice
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA174235
op_rights APPROVED FOR PUBLIC RELEASE
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