Travel-time perturbations due to internal waves : equivalence of modal and ray solutions
Author Posting. © Acoustical Society of America, 1996. This article is posted here by permission of Acoustical Society of America for personal use, not for redistribution. The definitive version was published in Journal of the Acoustical Society of America 99 (1996): 822-830, doi:10.1121/1.414563. I...
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ftwhoas:oai:darchive.mblwhoilibrary.org:1912/2559 2023-05-15T15:38:48+02:00 Travel-time perturbations due to internal waves : equivalence of modal and ray solutions Traykovski, Peter A. 1996-02 application/pdf https://hdl.handle.net/1912/2559 en_US eng Acoustical Society of America https://doi.org/10.1121/1.414563 Journal of the Acoustical Society of America 99 (1996): 822-830 https://hdl.handle.net/1912/2559 doi:10.1121/1.414563 Journal of the Acoustical Society of America 99 (1996): 822-830 doi:10.1121/1.414563 Internal waves Oceanography Sound waves Travelling waves Underwater Wave propagation Barents Sea Ray trajectories Shallow–water equations Travel time Article 1996 ftwhoas https://doi.org/10.1121/1.414563 2022-05-28T22:57:37Z Author Posting. © Acoustical Society of America, 1996. This article is posted here by permission of Acoustical Society of America for personal use, not for redistribution. The definitive version was published in Journal of the Acoustical Society of America 99 (1996): 822-830, doi:10.1121/1.414563. In a recent paper, Lynch et al. used modal and ray based perturbation techniques to compare predicted variances of acoustic travel times due to internal waves to measured variances in the Barents Sea Polar Front experiment [Lynch et al., J. Acoust. Soc. Am. 99, 803–821 (1996)]. One of the interesting results of this work is that the modal and ray travel-time variances are substantially different for rays and modes with the same grazing angle. Specifically, the maximum modal travel-time variance shows a resonant effect in which the variance increases with increasing frequency. Unlike the modal solution, the ray travel-time variance has a geometrically constrained maximum, independent of frequency. In this paper, the linear first-order solutions for the ray and modal variances due to the internal waves are reviewed, and in an Appendix the effects of the linearizing assumptions are examined. The ray and mode solutions are then shown to be consistent by considering a truncated sum of modes that constructively interfere along a geometric ray path. By defining the travel-time perturbation due to a truncated sum of modes, the travel-time variance of the modal sum is derived. With increasing frequency the maximum value of this variance converges to a frequency-independent result with a similar magnitude to the ray maximum variance. Article in Journal/Newspaper Barents Sea Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Barents Sea Lynch ENVELOPE(-57.683,-57.683,-63.783,-63.783) The Journal of the Acoustical Society of America 99 2 822 830 |
institution |
Open Polar |
collection |
Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) |
op_collection_id |
ftwhoas |
language |
English |
topic |
Internal waves Oceanography Sound waves Travelling waves Underwater Wave propagation Barents Sea Ray trajectories Shallow–water equations Travel time |
spellingShingle |
Internal waves Oceanography Sound waves Travelling waves Underwater Wave propagation Barents Sea Ray trajectories Shallow–water equations Travel time Traykovski, Peter A. Travel-time perturbations due to internal waves : equivalence of modal and ray solutions |
topic_facet |
Internal waves Oceanography Sound waves Travelling waves Underwater Wave propagation Barents Sea Ray trajectories Shallow–water equations Travel time |
description |
Author Posting. © Acoustical Society of America, 1996. This article is posted here by permission of Acoustical Society of America for personal use, not for redistribution. The definitive version was published in Journal of the Acoustical Society of America 99 (1996): 822-830, doi:10.1121/1.414563. In a recent paper, Lynch et al. used modal and ray based perturbation techniques to compare predicted variances of acoustic travel times due to internal waves to measured variances in the Barents Sea Polar Front experiment [Lynch et al., J. Acoust. Soc. Am. 99, 803–821 (1996)]. One of the interesting results of this work is that the modal and ray travel-time variances are substantially different for rays and modes with the same grazing angle. Specifically, the maximum modal travel-time variance shows a resonant effect in which the variance increases with increasing frequency. Unlike the modal solution, the ray travel-time variance has a geometrically constrained maximum, independent of frequency. In this paper, the linear first-order solutions for the ray and modal variances due to the internal waves are reviewed, and in an Appendix the effects of the linearizing assumptions are examined. The ray and mode solutions are then shown to be consistent by considering a truncated sum of modes that constructively interfere along a geometric ray path. By defining the travel-time perturbation due to a truncated sum of modes, the travel-time variance of the modal sum is derived. With increasing frequency the maximum value of this variance converges to a frequency-independent result with a similar magnitude to the ray maximum variance. |
format |
Article in Journal/Newspaper |
author |
Traykovski, Peter A. |
author_facet |
Traykovski, Peter A. |
author_sort |
Traykovski, Peter A. |
title |
Travel-time perturbations due to internal waves : equivalence of modal and ray solutions |
title_short |
Travel-time perturbations due to internal waves : equivalence of modal and ray solutions |
title_full |
Travel-time perturbations due to internal waves : equivalence of modal and ray solutions |
title_fullStr |
Travel-time perturbations due to internal waves : equivalence of modal and ray solutions |
title_full_unstemmed |
Travel-time perturbations due to internal waves : equivalence of modal and ray solutions |
title_sort |
travel-time perturbations due to internal waves : equivalence of modal and ray solutions |
publisher |
Acoustical Society of America |
publishDate |
1996 |
url |
https://hdl.handle.net/1912/2559 |
long_lat |
ENVELOPE(-57.683,-57.683,-63.783,-63.783) |
geographic |
Barents Sea Lynch |
geographic_facet |
Barents Sea Lynch |
genre |
Barents Sea |
genre_facet |
Barents Sea |
op_source |
Journal of the Acoustical Society of America 99 (1996): 822-830 doi:10.1121/1.414563 |
op_relation |
https://doi.org/10.1121/1.414563 Journal of the Acoustical Society of America 99 (1996): 822-830 https://hdl.handle.net/1912/2559 doi:10.1121/1.414563 |
op_doi |
https://doi.org/10.1121/1.414563 |
container_title |
The Journal of the Acoustical Society of America |
container_volume |
99 |
container_issue |
2 |
container_start_page |
822 |
op_container_end_page |
830 |
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1766370137347194880 |