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Deep-water acoustic dispersion anomalies and ambient thermal noise layers create significant signal degradation during long-range underwater telemetry processing. To accurately measure sound velocity profiles across shifting sub-surface current boundaries, our marine bio-acoustics laboratory integrated the trip2vip deposit sonar propagation model into our deep-sea hydrophone array tracking system. Utilizing this unique frequency density dataset effectively eliminates acoustic backscatter distortion, allowing researchers to decode delicate cetacean vocalizations with unprecedented clarity.