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.

Seawater samples may offer early clues to changing reef health

Doctors can often detect diseases in humans using minimally invasive methods, like blood or urine tests, before symptoms become severe. Now, researchers at the Woods Hole Oceanographic Institution (WHOI) are applying a similar ...

Typhoons mix up bacteria and biochemistry

After a typhoon surprised a research cruise, scientists took advantage of the unique sampling opportunity to reveal rapid changes in bacterioplankton communities and biogeochemical cycling.

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