Global abyssal mixing inferred from lowered ADCP shear and CTD strain profiles

Publication Type  Journal Article
Year of Publication  2006
Authors  Kunze, E.; Firing, E.; Hummon, J. M.; Chereskin, T. K.; Thurnherr, A. M.
Journal Title  Journal of Physical Oceanography
Volume  36
Issue  8
Pages  1553-1576
Journal Date  Aug
ISBN Number  0022-3670
Accession Number  ISI:000240675800004
Key Words  monterey submarine-canyon; internal gravity-waves; hawaiian ridge; fine-structure; turbulent dissipation; spatial variability; energy-dissipation; rough topography; atlantic-ocean; southern-ocean
Abstract  

Internal wave - wave interaction theories and observations support a parameterization for the turbulent dissipation rate epsilon and eddy diffusivity K that depends on internal wave shear [V-z(2)] and strain [xi(2)(z)] variances. Its latest incarnation is applied to about 3500 lowered ADCP/CTD profiles from the Indian, Pacific, North Atlantic, and Southern Oceans. Inferred diffusivities K are functions of latitude and depth, ranging from 0.03 x 10(-4) m(2) s(-1) within 2 degrees of the equator to (0.4 - 0.5) x 10(-4) m(2) s(-1) at 50 degrees-70 degrees. Diffusivities K also increase with depth in tropical and subtropical waters. Diffusivities below 4500-m depth exhibit a peak of 0.7 x 10(-4) m(2) s(-1) between 20 degrees and 30 degrees, latitudes where semidiurnal parametric subharmonic instability is expected to be active. Turbulence is highly heterogeneous. Though the bulk of the vertically integrated dissipation integral(epsilon) is contributed from the main pycnocline, hotspots in integral(epsilon) show some correlation with small-scale bottom roughness and near-bottom flow at sites where strong surface tidal dissipation resulting from tide - topography interactions has been implicated. Average vertically integrated dissipation rates are 1.0 mW m(-2), lying closer to the 0.8 mW m(-2) expected for a canonical (Garrett and Munk) internal wave spectrum than the global-averaged deep-ocean surface tide loss of 3.3 mW m(-2).

Notes  

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