Abstract:Ray-based acoustical tomography typically provides estimates of local ocean sound speed profile (SSP) fluctuations from precise measurements of acoustic travel times (AT) fluctuations (with respect to a reference environment) between multiple sources and receiver arrays along with a model of the ray propagation in the reference (i.e., fluctuation-free) environment. Classically, inverting the forward model (if available) yielding SSPs from ATs can be done by computing the pseudo-inverse (expensive) or using an … Show more
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