Acoustic travel time perturbations due to an internal tide and internal wave field in the Barents Sea

Submitted in partial fulfillment of the requirements for the degree of Ocean Engineer at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution August 1993 Travel time perturbations of adiabatic normal modes due to an internal tide and internal mode field in the Baren...

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Main Author: Ray, Douglas S.
Format: Thesis
Language:English
Published: Massachusetts Institute of Technology and Woods Hole Oceanographic Institution 1993
Subjects:
Online Access:https://hdl.handle.net/1912/5539
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spelling ftwhoas:oai:darchive.mblwhoilibrary.org:1912/5539 2023-05-15T15:38:12+02:00 Acoustic travel time perturbations due to an internal tide and internal wave field in the Barents Sea Ray, Douglas S. Barents Sea 1993-08 application/pdf https://hdl.handle.net/1912/5539 en_US eng Massachusetts Institute of Technology and Woods Hole Oceanographic Institution WHOI Theses https://hdl.handle.net/1912/5539 doi:10.1575/1912/5539 doi:10.1575/1912/5539 Internal waves Ocean circulation Acoustic surface waves Thesis 1993 ftwhoas https://doi.org/10.1575/1912/5539 2022-05-28T22:58:43Z Submitted in partial fulfillment of the requirements for the degree of Ocean Engineer at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution August 1993 Travel time perturbations of adiabatic normal modes due to an internal tide and internal mode field in the Barents Sea are examined. A formalism for the travel time perturbation due to a change in sound speed is presented. Internal tide and internal wave amplitude spectra are calculated from Brancker temperature loggers which were deployed on moorings in the Barents Sea during the August 1992 Barents Sea Polar Front Experiment. In particular, the first three internal wave mode amplitudes are estimated from the four Brancker temperature loggers on the southwest mooring of the array. Modal perturbations in acoustic pulse travel time and the travel time covariance are calculated and compared for consistency to a simple ray model. These perturbations are small for the modal arrivals that the vertical acoustic array which was deployed is expected to resolve. The third internal wave mode has the largest impact on the acoustic arrivals, per unit amplitude, but the first internal wave mode dominates the scattering due to having a much larger amplitude overall. Thesis Barents Sea Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Barents Sea Woods Hole, MA
institution Open Polar
collection Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server)
op_collection_id ftwhoas
language English
topic Internal waves
Ocean circulation
Acoustic surface waves
spellingShingle Internal waves
Ocean circulation
Acoustic surface waves
Ray, Douglas S.
Acoustic travel time perturbations due to an internal tide and internal wave field in the Barents Sea
topic_facet Internal waves
Ocean circulation
Acoustic surface waves
description Submitted in partial fulfillment of the requirements for the degree of Ocean Engineer at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution August 1993 Travel time perturbations of adiabatic normal modes due to an internal tide and internal mode field in the Barents Sea are examined. A formalism for the travel time perturbation due to a change in sound speed is presented. Internal tide and internal wave amplitude spectra are calculated from Brancker temperature loggers which were deployed on moorings in the Barents Sea during the August 1992 Barents Sea Polar Front Experiment. In particular, the first three internal wave mode amplitudes are estimated from the four Brancker temperature loggers on the southwest mooring of the array. Modal perturbations in acoustic pulse travel time and the travel time covariance are calculated and compared for consistency to a simple ray model. These perturbations are small for the modal arrivals that the vertical acoustic array which was deployed is expected to resolve. The third internal wave mode has the largest impact on the acoustic arrivals, per unit amplitude, but the first internal wave mode dominates the scattering due to having a much larger amplitude overall.
format Thesis
author Ray, Douglas S.
author_facet Ray, Douglas S.
author_sort Ray, Douglas S.
title Acoustic travel time perturbations due to an internal tide and internal wave field in the Barents Sea
title_short Acoustic travel time perturbations due to an internal tide and internal wave field in the Barents Sea
title_full Acoustic travel time perturbations due to an internal tide and internal wave field in the Barents Sea
title_fullStr Acoustic travel time perturbations due to an internal tide and internal wave field in the Barents Sea
title_full_unstemmed Acoustic travel time perturbations due to an internal tide and internal wave field in the Barents Sea
title_sort acoustic travel time perturbations due to an internal tide and internal wave field in the barents sea
publisher Massachusetts Institute of Technology and Woods Hole Oceanographic Institution
publishDate 1993
url https://hdl.handle.net/1912/5539
op_coverage Barents Sea
geographic Barents Sea
geographic_facet Barents Sea
genre Barents Sea
genre_facet Barents Sea
op_source doi:10.1575/1912/5539
op_relation WHOI Theses
https://hdl.handle.net/1912/5539
doi:10.1575/1912/5539
op_doi https://doi.org/10.1575/1912/5539
op_publisher_place Woods Hole, MA
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