Mixing on the continental slope of the southern Weddell Sea

• Published in: Journal of Geophysical Research
• Main Authors: Daae, Kjersti L., Fer, Ilker, Abrahamsen, E. Povl
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: American Geophysical Union 2009
• Subjects: Marine Sciences; Earth Sciences; Weddell Sea; Weddell
• Online Access: http://nora.nerc.ac.uk/id/eprint/7616/; https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2008JC005259

Shipboard hydrography and current profiles collected in 2003 and time series from moored current meters deployed in late 1990s are analyzed to study the variability of mixing in the southeastern Weddell Sea. Profiles of eddy diffusivity Kρ are inferred from finescale shear (vertical derivative of horizontal velocity) and strain (vertical derivative of isopycnal displacement) variance using parameterizations which relate the internal wave energy to the dissipation rate at small scales. The highest mixing rates are seen near the bottom where the eddy diffusivities are elevated by one order of magnitude from those in the interior and exceed 10^−4 m^2 s^−1. The observations show latitudinal variability in Kρ, particularly near the bottom, where Kρ significantly increases near 74° 28' S, the critical latitude for lunar semi-diurnal (M2) tides. In this region, the critical latitude coincides with near-critical topography on the upper continental slope, a situation which favors generation of M2 internal waves. Consistent with the results from finescale shear and strain parameterizations, which indicate highest bottom diffusivities near the critical latitude, independent analysis of current time series from moored instruments shows a thickening of the frictional bottom boundary layer near the critical latitude. Semidiurnal tidal dynamics at the upper continental slope together with the critical latitude effects lead to mixing that might significantly affect the regional heat budget and the circulation in the study area.