1987
DOI: 10.1121/1.394571
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Eigenray finding and time series simulation in a layered-bottom ocean

Abstract: A ray theory approach for simulating the propagation of broadband signals interacting with a layered ocean bottom is presented. The range-invariant environment consists of the ocean and an arbitrary number of bottom layers. Each bottom layer has profiles of compressional and shear wave velocity, attenuation, and density. Eigenrays, including those with multiple interactions and refractions in the ocean and bottom layering, are found using a thorough and efficient algorithm based on an analysis of the sound vel… Show more

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Cited by 47 publications
(12 citation statements)
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“…It may be possible to use a ray tracer if the acoustic bottom interactions are treated correctly. 28,29 ͑2͒ Geometry-The ideal measurement geometry will also need to be determined as it is likely that parameters like array length, tow depths, and signal types will need to be optimized to improve estimates of the seabed properties. ͑3͒ Cost functions-Cost functions have different sensitivities that de-TABLE III.…”
Section: Discussionmentioning
confidence: 99%
“…It may be possible to use a ray tracer if the acoustic bottom interactions are treated correctly. 28,29 ͑2͒ Geometry-The ideal measurement geometry will also need to be determined as it is likely that parameters like array length, tow depths, and signal types will need to be optimized to improve estimates of the seabed properties. ͑3͒ Cost functions-Cost functions have different sensitivities that de-TABLE III.…”
Section: Discussionmentioning
confidence: 99%
“…24 A seabed containing many thin sediment layers is known to cause distortion of broadband signals resulting from multiple reflections of acoustic rays with sub-bottom interfaces. 26 However, at low frequencies, the long wavelengths are insensitive to the details of thin layers and interact with an effectively continuous velocity profile. The accuracy of describing the layered ooze found in the Catoche Tongue with a simplified sediment representation was assessed by comparing the modeled time series of the direct (non-horizontally refracted) arrivals in a 5 Hz band centered at 25 Hz using a 2D normal-mode model.…”
Section: B Environmental Representationmentioning
confidence: 99%
“…Many different techniques in this category tend to be informal and often partially empirical solution based. One example of the solution for semi-coherent transmission loss calculation is given by [13] …”
Section: Transmission Lossmentioning
confidence: 99%