Internal tides and turbulence along the 3000m isobath of the Hawaiian Ridge

Full-depth velocity and density profiles taken along the 3000-m isobath characterize the semidiurnal internal tide and bottom-intensified turbulence along the Hawaiian Ridge. Observations reveal baroclinic energy fluxes of 21 5 kW m1 radiating from French Frigate Shoals, 17 2.5 kW m1 from Kauai Channel west of Oahu, and 13 3.5 kW m1 from west of Nihoa Island. Weaker fluxes of 1–4 2 kW m1 radiate from the region near Necker Island and east of Nihoa Island. Observed off-ridge energy fluxes generally agree to within a factor of 2 with those produced by a tidally forced numerical model. Average turbulent diapycnal diffusivity K is (0.5–1) 104 m2 s–1 above 2000 m, increasing exponentially to 20 104 m2 s–1 near the bottom. Microstructure values agree well with those inferred from a finescale internal wave-based parameterization. A linear relationship between the vertically integrated energy flux and ver-tically integrated turbulent dissipation rate implies that dissipative length scales for the radiating internal tide exceed 1000 km. 1