Abstract
The adiabatic mode parabolic equation is generalized to the case of an ocean overlying an elastic bottom. This three-dimensional model is valid when the medium varies sufficiently gradually with the horizontal coordinates so that both coupling of energy between modes and the azimuthal component of displacement may be neglected. The efficiency of the model is demonstrated by applying it to solve a global-acoustics problem involving diffraction by the Hawaiian Islands.
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© 1995 Springer Science+Business Media Dordrecht
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Orris, G.J., Collins, M.D., Deane, G.B., Porter, M.B. (1995). Three-Dimensional Sound Propagation in an Ocean Overlying an Elastic Bottom. In: Diachok, O., Caiti, A., Gerstoft, P., Schmidt, H. (eds) Full Field Inversion Methods in Ocean and Seismo-Acoustics. Modern Approaches in Geophysics, vol 12. Springer, Dordrecht. https://doi.org/10.1007/978-94-015-8476-0_12
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DOI: https://doi.org/10.1007/978-94-015-8476-0_12
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