Multiple Surface Scattering from the Ice Covered Arctic Ocean.

The range dependent boundary condition imposed by a rough ice surface serves to couple the normal-modes of an underwater acoustic field. Beginning with the parabolic wave equation, the solution is expanded in terms of normal-mode depth functions modulated by random amplitudes. A system of master equ...

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Main Authors: Beilis,A, Tappert,F D, Kutschale,H W
Other Authors: LAMONT-DOHERTY GEOLOGICAL OBSERVATORY PALISADES N Y
Format: Text
Language:English
Published: 1979
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA069843
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA069843
id ftdtic:ADA069843
record_format openpolar
spelling ftdtic:ADA069843 2023-05-15T14:55:15+02:00 Multiple Surface Scattering from the Ice Covered Arctic Ocean. Beilis,A Tappert,F D Kutschale,H W LAMONT-DOHERTY GEOLOGICAL OBSERVATORY PALISADES N Y 1979-03 text/html http://www.dtic.mil/docs/citations/ADA069843 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA069843 en eng http://www.dtic.mil/docs/citations/ADA069843 Availability: Document partially illegible. DTIC AND NTIS Snow Ice and Permafrost Acoustics *ICE *ACOUSTIC SCATTERING *UNDERWATER ACOUSTICS COMPUTER PROGRAMS WIND ACOUSTIC SIGNALS MARINE METEOROLOGY ANTISUBMARINE WARFARE ARCTIC OCEAN Text 1979 ftdtic 2016-02-20T16:08:24Z The range dependent boundary condition imposed by a rough ice surface serves to couple the normal-modes of an underwater acoustic field. Beginning with the parabolic wave equation, the solution is expanded in terms of normal-mode depth functions modulated by random amplitudes. A system of master equations for the quantities an (r) an * (r) is derived, where the a sub n (r) are the normal mode amplitudes, and the brackets indicate an ensemble average. The master equations determine the mean power in each mode as a function of range, describing the transfer of energy between modes. Explicit relations for the coupling coefficients are obtained in terms of the spectrum of the rough surface. Transmission loss, intensity redistribution and the approach to equipartition of energy as functions of range and depth are obtained numerically. (Author) Prepared in cooperation with New York Univ., NY. Text 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
*ICE
*ACOUSTIC SCATTERING
*UNDERWATER ACOUSTICS
COMPUTER PROGRAMS
WIND
ACOUSTIC SIGNALS
MARINE METEOROLOGY
ANTISUBMARINE WARFARE
ARCTIC OCEAN
spellingShingle Snow
Ice and Permafrost
Acoustics
*ICE
*ACOUSTIC SCATTERING
*UNDERWATER ACOUSTICS
COMPUTER PROGRAMS
WIND
ACOUSTIC SIGNALS
MARINE METEOROLOGY
ANTISUBMARINE WARFARE
ARCTIC OCEAN
Beilis,A
Tappert,F D
Kutschale,H W
Multiple Surface Scattering from the Ice Covered Arctic Ocean.
topic_facet Snow
Ice and Permafrost
Acoustics
*ICE
*ACOUSTIC SCATTERING
*UNDERWATER ACOUSTICS
COMPUTER PROGRAMS
WIND
ACOUSTIC SIGNALS
MARINE METEOROLOGY
ANTISUBMARINE WARFARE
ARCTIC OCEAN
description The range dependent boundary condition imposed by a rough ice surface serves to couple the normal-modes of an underwater acoustic field. Beginning with the parabolic wave equation, the solution is expanded in terms of normal-mode depth functions modulated by random amplitudes. A system of master equations for the quantities an (r) an * (r) is derived, where the a sub n (r) are the normal mode amplitudes, and the brackets indicate an ensemble average. The master equations determine the mean power in each mode as a function of range, describing the transfer of energy between modes. Explicit relations for the coupling coefficients are obtained in terms of the spectrum of the rough surface. Transmission loss, intensity redistribution and the approach to equipartition of energy as functions of range and depth are obtained numerically. (Author) Prepared in cooperation with New York Univ., NY.
author2 LAMONT-DOHERTY GEOLOGICAL OBSERVATORY PALISADES N Y
format Text
author Beilis,A
Tappert,F D
Kutschale,H W
author_facet Beilis,A
Tappert,F D
Kutschale,H W
author_sort Beilis,A
title Multiple Surface Scattering from the Ice Covered Arctic Ocean.
title_short Multiple Surface Scattering from the Ice Covered Arctic Ocean.
title_full Multiple Surface Scattering from the Ice Covered Arctic Ocean.
title_fullStr Multiple Surface Scattering from the Ice Covered Arctic Ocean.
title_full_unstemmed Multiple Surface Scattering from the Ice Covered Arctic Ocean.
title_sort multiple surface scattering from the ice covered arctic ocean.
publishDate 1979
url http://www.dtic.mil/docs/citations/ADA069843
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA069843
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Ice
permafrost
genre_facet Arctic
Arctic Ocean
Ice
permafrost
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA069843
op_rights Availability: Document partially illegible.
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