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MACKINNON, J. A; ALFORD, M. H; PINKEL, Rob; KLYMAK, Jody; ZHONGXIANG ZHAO
Journal of physical oceanography, 2013, 2013-01-01, 20130101, Letnik: 43, Številka: 1Journal Article
Abstract Turbulent mixing rates are inferred from measurements spanning 25°–37°N in the Pacific Ocean. The observations were made as part of the Internal Waves Across the Pacific experiment, designed to investigate the long-range fate of the low-mode internal tide propagating north from Hawaii. Previous and companion results argue that, near a critical latitude of 29°N, the internal tide loses energy to high-mode near-inertial motions through parametric subharmonic instability. Here, the authors estimate mixing from several variations of the finescale shear–strain parameterization, as well as Thorpe-scale analysis of overturns. Though all estimated diffusivities are modest in magnitude, average diffusivity in the top kilometer shows a factor of 2–4 elevation near and equatorward of 29°N. However, given intrinsic uncertainty and the strong temporal variability of diffusivity observed in long mooring records, the meridional mixing pattern is found to be near the edge of statistical significance.
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JCR | SNIP | JCR | SNIP | JCR | SNIP | JCR | SNIP |
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