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dc.contributor.authorZiomek, Lawrence J.
dc.date.accessioned2018-09-19T16:25:20Z
dc.date.available2018-09-19T16:25:20Z
dc.date.issued1982
dc.identifier.citationThe Journal of the Acoustical Society of America 71, 1487 (1982); https://doi.org/10.1121/1.387847en_US
dc.identifier.urihttp://hdl.handle.net/10945/59969
dc.descriptionThe article of record as published may be found at https://doi.org/10.1121/1.387847en_US
dc.description.abstractThree second‐order functions which characterize the ocean surface‐scatter communication channel are derived from the transfer function of the ocean surface. These second‐order functions include the two‐frequency correlation function or the two‐frequency mutual coherence function, the scattering function, and the power spectral density function of the scattered acoustic pressure field. These functions are shown to be dependent upon the general form of the directional wavenumber spectrum. Both the slightly rough and very rough surface cases are included. The interrelationships which exist amongst these functions are demonstrated. As an example, the power spectral density function is computed for the very rough surface case using the Neumann–Pierson directional wavenumber spectrum.en_US
dc.description.sponsorshipThe work described in this paper was supported by NAVSEA Undersea Weapons Guidance and Control Block, Code NSEA 63R-14.en_US
dc.publisherAcoustical Society of Americaen_US
dc.rightsThis publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States.en_US
dc.titleGeneralized Kirchhoff approach to the ocean surface‐scatter communication channel. Part II: Second‐order functionsen_US
dc.typeArticleen_US
dc.contributor.departmentElectrical Engineeringen_US


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