Page 4: Research news on ocean mixing

Ocean mixing is a physical oceanographic phenomenon encompassing the turbulent and wave-driven processes that irreversibly redistribute heat, salt, momentum, and biogeochemical tracers within the ocean interior and boundary layers. It is mediated by shear instability, double-diffusive convection, internal waves (including internal tides), and boundary-generated turbulence, and is quantified using parameters such as diapycnal and isopycnal diffusivities. Ocean mixing regulates the vertical exchange between the surface and deep ocean, controls stratification and overturning circulation, influences climate-relevant heat and carbon storage, and sets nutrient supply to the euphotic zone, thereby coupling physical dynamics with marine biogeochemistry.

After the fury, hurricanes can leave a lasting mark on deep ocean

The impact of hurricanes when they travel over land, or when they affect ships or oil-drilling platforms, are quite well understood. But these huge cyclones also stir up the ocean itself, with consequences that are relatively ...

page 4 from 5