Research news on upwelling

Upwelling is an oceanographic phenomenon in which deeper, typically colder and nutrient-rich water is transported toward the surface, primarily driven by wind-induced divergence of surface waters and the action of the Coriolis force. Along eastern ocean boundaries, along-equatorward winds generate Ekman transport that moves surface water offshore, causing compensatory upward flow from depth. Equatorial upwelling occurs where trade winds cause divergence of surface waters on either side of the equator. Upwelling strongly influences primary productivity, biogeochemical cycling, and thermal structure in the upper ocean, and is a key control on regional climate and fisheries in major eastern boundary current systems.

Ocean fronts revealed as key players in Earth's carbon cycle

Narrow bands of ocean covering just over one-third of the world's seas are responsible for absorbing nearly three-quarters of the carbon dioxide that oceans pull from the atmosphere, new research shows. The study, published ...

Scientists detect deep Earth pulses beneath Africa

Research led by Earth scientists at the University of Southampton has uncovered evidence of rhythmic surges of molten mantle rock rising from deep within the Earth beneath Africa. These pulses are gradually tearing the continent ...

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