Abstract
The self-starter is implemented by the method of undetermined coefficients for ocean acoustics problems involving elastic sediment layers. This approach is efficient when the ocean bottom can be approximated by a relatively small number of homogeneous layers. For many problems, the self-starter only requires on the order of 10 wave number samples to provide accurate solutions at ranges on the order of 10 wavelengths. The geoacoustic inverse problem can be solved in nearly real time with this approach, which can generate on the order of a thousand forward solutions per second on the current generation of desk-top computers.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
