Published In

JASA Express Letters

Document Type

Article

Publication Date

7-16-2026

Subjects

Marine sediments, sound speed profiles

Abstract

Marine sediment sound speed profiles in the upper ten meters are generally assumed to be constant with time. Models predict that substantive changes occur because of thermal conduction from seasonally varying bottom water temperature. However, definitive measurements have been lacking. In this work, sediment sound speed profiles obtained during different seasons show significant differences in the upper 9 m of mud at the New England Patch. Gradients in late March 2017 are 6.0 s−1 and in early October 2025, 2.6 s−1. This change is shown to have a significant impact on acoustic propagation.

Rights

Copyright (c) 2026 The Authors

Creative Commons License

This work is licensed under a Creative Commons Attribution 4.0 International License.

DOI

10.1121/10.0044366

Persistent Identifier

https://archives.pdx.edu/ds/psu/45010

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