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.

NASA satellites reveal major ocean nutrient stress

A new study combining NASA satellite observations, ocean surveys and genetic testing of marine microorganisms found evidence that warming ocean waters may be limiting nutrient availability across much of the global ocean. ...

Scientists identify hidden accelerant in Antarctic ice loss

For years, scientists have warned that melting Antarctic ice could push sea levels dangerously higher by the end of this century. But a new study led by University of Maryland scientist Madeleine Youngs suggests those warnings ...

Were Martian tides strong enough to shape its ancient landscape?

You're an anaerobic microbe sunbathing on a Martian beach billions of years ago listening to the small waves hit the shoreline as you take in the perchlorates in the Martian regolith. This is because while Mars is warm and ...

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