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Deep ocean sound speed characteristics passively derived from the ambient acoustic noise field

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Delft University of Technology

Deep ocean sound speed characteristics passively derived from the ambient acoustic

noise field

Evers, Laeslo G; Wapenaar, Kees; Heaney, Kevin D; Snellen, Mirjam

Publication date 2016

Document Version Final published version Citation (APA)

Evers, L. G., Wapenaar, K., Heaney, K. D., & Snellen, M. (2016). Deep ocean sound speed characteristics passively derived from the ambient acoustic noise field. Abstract from AGU fall meeting 2016, San

Francisco, United States. Important note

To cite this publication, please use the final published version (if applicable). Please check the document version above.

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This work is downloaded from Delft University of Technology.

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04/04/19 22:33 2016 AGU Fall Meeting

Page 1 of 2 https://agu.confex.com/agu/fm16/meetingapp.cgi/

S52A-07: Deep ocean sound speed characteristics passively derived from the

ambient acoustic noise field

Friday, 16 December 2016 12:05 - 12:20

Moscone South - 305

The propagation of acoustic waves in the ocean strongly depends on the temperature. Low frequency acoustic waves can penetrate the ocean down to depths where few in-situ measurements are available. It is therefore attractive to obtain a measure of the deep ocean temperature from acoustic waves. The latter is especially true if the ambient acoustic noise field can be used instead of deterministic transient signals. In this study the acoustic velocity, and hence the temperature, is derived in an interferometric approach from hydrophone array recordings. The arrays were separated by over 125 km, near Ascension Island in the Atlantic Ocean, at a depth of 800m. Furthermore, the

dispersive characteristics of the deep ocean sound channel are resolved based on the retrieved lag times for different modes. In addition, it is shown how the resolution of the interferometric approach can be increased by cross

correlating array beams rather than recordings from single-sensor pairs. The observed acoustic lag times between the arrays corresponds well to modeled values, based on full-wave modeling through best-known oceanic models.

Authors

Laeslo G Evers *

Royal Netherlands Meteorological Institute

Cornelis P A Wapenaar

Delft University of Technology

Kevin D Heaney

OASIS Inc.

Mirjam Snellen

Delft University of Technology

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