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...
Main Author: | |
---|---|
Other Authors: | |
Format: | Text |
Language: | English |
Published: |
1986
|
Subjects: | |
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 |
_version_ |
1766324149275328512 |