Seismic imaging of a thermohaline staircase in the western tropical North Atlantic
© The Authors, 2010. This article is distributed under the terms of the Creative Commons Attribution 3.0 License. The definitive version was published in Ocean Science 6 (2010): 621-631, doi:10.5194/os-6-621-2010. Multichannel seismic data acquired in the Lesser Antilles in the western tropical Nort...
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ftwhoas:oai:darchive.mblwhoilibrary.org:1912/3915 2023-05-15T17:32:04+02:00 Seismic imaging of a thermohaline staircase in the western tropical North Atlantic Fer, Ilker Nandi, Papia Holbrook, W. Steven Schmitt, Raymond W. Paramo, Pedro 2010-07-02 application/pdf https://hdl.handle.net/1912/3915 en eng Copernicus Publications on behalf of the European Geosciences Union https://doi.org/10.5194/os-6-621-2010 Ocean Science 6 (2010): 621-631 https://hdl.handle.net/1912/3915 doi:10.5194/os-6-621-2010 Attribution 3.0 Unported http://creativecommons.org/licenses/by/3.0/ CC-BY Ocean Science 6 (2010): 621-631 doi:10.5194/os-6-621-2010 Article 2010 ftwhoas https://doi.org/10.5194/os-6-621-2010 2022-05-28T22:58:07Z © The Authors, 2010. This article is distributed under the terms of the Creative Commons Attribution 3.0 License. The definitive version was published in Ocean Science 6 (2010): 621-631, doi:10.5194/os-6-621-2010. Multichannel seismic data acquired in the Lesser Antilles in the western tropical North Atlantic indicate that the seismic reflection method has imaged an oceanic thermohaline staircase. Synthetic acoustic modeling using measured density and sound speed profiles corroborates inferences from the seismic data. In a small portion of the seismic image, laterally coherent, uniform layers are present at depths ranging from 550–700 m and have a separation of ~20 m, with thicknesses increasing with depth. The reflection coefficient, a measure of the acoustic impedance contrasts across these reflective interfaces, is one order of magnitude greater than background noise. Hydrography sampled in previous surveys suggests that the layers are a permanent feature of the region. Spectral analysis of layer horizons in the thermohaline staircase indicates that internal wave activity is anomalously low, suggesting weak internal wave-induced turbulence. Results from two independent measurements, the application of a finescale parameterization to observed high-resolution velocity profiles and direct measurements of turbulent dissipation rate, confirm these low levels of turbulence. The lack of internal wave-induced turbulence may allow for the maintenance of the staircase or may be due to suppression by the double-diffusive convection within the staircase. Our observations show the potential for seismic oceanography to contribute to an improved understanding of occurrence rates and the geographical distribution of thermohaline staircases, and should thereby improve estimates of vertical mixing rates ascribable to salt fingering in the global ocean. This research was supported by NSF grant OCE-0221366 and ONR grant ONR-N000140410585 to Holbrook, NSF grant OCE-0647573 to Schmitt and the University of Wyoming Graduate ... Article in Journal/Newspaper North Atlantic Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Ocean Science 6 3 621 631 |
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Open Polar |
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Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) |
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ftwhoas |
language |
English |
description |
© The Authors, 2010. This article is distributed under the terms of the Creative Commons Attribution 3.0 License. The definitive version was published in Ocean Science 6 (2010): 621-631, doi:10.5194/os-6-621-2010. Multichannel seismic data acquired in the Lesser Antilles in the western tropical North Atlantic indicate that the seismic reflection method has imaged an oceanic thermohaline staircase. Synthetic acoustic modeling using measured density and sound speed profiles corroborates inferences from the seismic data. In a small portion of the seismic image, laterally coherent, uniform layers are present at depths ranging from 550–700 m and have a separation of ~20 m, with thicknesses increasing with depth. The reflection coefficient, a measure of the acoustic impedance contrasts across these reflective interfaces, is one order of magnitude greater than background noise. Hydrography sampled in previous surveys suggests that the layers are a permanent feature of the region. Spectral analysis of layer horizons in the thermohaline staircase indicates that internal wave activity is anomalously low, suggesting weak internal wave-induced turbulence. Results from two independent measurements, the application of a finescale parameterization to observed high-resolution velocity profiles and direct measurements of turbulent dissipation rate, confirm these low levels of turbulence. The lack of internal wave-induced turbulence may allow for the maintenance of the staircase or may be due to suppression by the double-diffusive convection within the staircase. Our observations show the potential for seismic oceanography to contribute to an improved understanding of occurrence rates and the geographical distribution of thermohaline staircases, and should thereby improve estimates of vertical mixing rates ascribable to salt fingering in the global ocean. This research was supported by NSF grant OCE-0221366 and ONR grant ONR-N000140410585 to Holbrook, NSF grant OCE-0647573 to Schmitt and the University of Wyoming Graduate ... |
format |
Article in Journal/Newspaper |
author |
Fer, Ilker Nandi, Papia Holbrook, W. Steven Schmitt, Raymond W. Paramo, Pedro |
spellingShingle |
Fer, Ilker Nandi, Papia Holbrook, W. Steven Schmitt, Raymond W. Paramo, Pedro Seismic imaging of a thermohaline staircase in the western tropical North Atlantic |
author_facet |
Fer, Ilker Nandi, Papia Holbrook, W. Steven Schmitt, Raymond W. Paramo, Pedro |
author_sort |
Fer, Ilker |
title |
Seismic imaging of a thermohaline staircase in the western tropical North Atlantic |
title_short |
Seismic imaging of a thermohaline staircase in the western tropical North Atlantic |
title_full |
Seismic imaging of a thermohaline staircase in the western tropical North Atlantic |
title_fullStr |
Seismic imaging of a thermohaline staircase in the western tropical North Atlantic |
title_full_unstemmed |
Seismic imaging of a thermohaline staircase in the western tropical North Atlantic |
title_sort |
seismic imaging of a thermohaline staircase in the western tropical north atlantic |
publisher |
Copernicus Publications on behalf of the European Geosciences Union |
publishDate |
2010 |
url |
https://hdl.handle.net/1912/3915 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Ocean Science 6 (2010): 621-631 doi:10.5194/os-6-621-2010 |
op_relation |
https://doi.org/10.5194/os-6-621-2010 Ocean Science 6 (2010): 621-631 https://hdl.handle.net/1912/3915 doi:10.5194/os-6-621-2010 |
op_rights |
Attribution 3.0 Unported http://creativecommons.org/licenses/by/3.0/ |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.5194/os-6-621-2010 |
container_title |
Ocean Science |
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6 |
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3 |
container_start_page |
621 |
op_container_end_page |
631 |
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1766129999938584576 |