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dc.contributor.authorFer, Ilker  Concept link
dc.contributor.authorNandi, Papia  Concept link
dc.contributor.authorHolbrook, W. Steven  Concept link
dc.contributor.authorSchmitt, Raymond W.  Concept link
dc.contributor.authorParamo, Pedro  Concept link
dc.date.accessioned2010-09-20T13:42:29Z
dc.date.available2010-09-20T13:42:29Z
dc.date.issued2010-07-02
dc.identifier.citationOcean Science 6 (2010): 621-631en_US
dc.identifier.urihttps://hdl.handle.net/1912/3915
dc.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.en_US
dc.description.abstractMultichannel 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.en_US
dc.description.sponsorshipThis 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 School Women and Minority Fellowship to Nandi.en_US
dc.format.mimetypeapplication/pdf
dc.language.isoenen_US
dc.publisherCopernicus Publications on behalf of the European Geosciences Unionen_US
dc.relation.urihttps://doi.org/10.5194/os-6-621-2010
dc.rightsAttribution 3.0 Unported*
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/*
dc.titleSeismic imaging of a thermohaline staircase in the western tropical North Atlanticen_US
dc.typeArticleen_US
dc.identifier.doi10.5194/os-6-621-2010


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Attribution 3.0 Unported
Except where otherwise noted, this item's license is described as Attribution 3.0 Unported