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May 14, 2026The Journal of the Acoustical Society of America0 citations

Retrieval of empirical Green’s functions from ambient sound recorded by deep-water receivers during the 2023–2024 NESMA experiment

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TTT W TanOGOleg A. GodinGGGanesh Gopalakrishnan

Key Points

  • This research aims to retrieve acoustic empirical Green’s functions from ambient sound recorded at deep-water sites during the NESMA experiments.
  • Deployed Moored Autonomous Noise Recorders (MANRs) near the Atlantis II Seamounts for 2 months in 2023 and 6 months in 2024.
  • Utilized sub-millisecond timing accuracy from atomic clocks to record ambient sound.
  • Stacked cross-correlation functions from approximately 100 hours of recordings to identify stable EGFs.
  • Produced empirical Green’s functions showing stable causal and acausal direct arrivals in the 15-50 Hz frequency band.
  • Tracked temporal evolution of acoustic travel time revealing information on sound speed and flow velocity.
  • Compared acoustic observations to tide-resolving MITgcm hydrodynamic simulations, indicating environmental variability.

Abstract

During the 2023 and 2024 New England Sea Mounts Acoustics (NESMA) experiments, the Naval Postgraduate School deployed a network of near-bottom Moored Autonomous Noise Recorders (MANRs) near the Atlantis II Seamounts. MANRs recorded ambient sound continuously for 2 months in 2023 and 6 months in 2024. Sub-millisecond timing accuracy was maintained with on-board chip-scale atomic clocks. This paper investigates the retrieval of acoustic empirical Green’s functions (EGFs) from cross-correlations of ambient sound simultaneously recorded by MANR#2 and MANR#3 located on steep seamount flanks and MANR#4 located on an abyssal plain. MANRs were located 4 m above the seafloor at depths of 2994, 4067, and 4443 m, respectively. Stacking cross-correlation functions from approximately 100 h of noise recordings is found to produce EGFs with stable causal and acausal direct arrivals in the 15–50 Hz frequency band. We then track the temporal evolution of the reciprocal and non-reciprocal components of the passively measured acoustic travel time, which contain information about the evolution of sound speed and flow velocity along the propagation path. Acoustic observations of the environmental variability in deep water in the vicinity of Atlantis II Seamounts are compared to tide-resolving MITgcm hydrodynamic simulations. Work supported by ONR.

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Cite This Study

Tan et al. (2025) studied this question.

synapsesocial.com/papers/6a0567bca550a87e60a1fe0dhttps://doi.org/10.1121/10.0041592
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