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.

El Niño is underway, satellite observations show

El Niño, characterized by warmer-than-normal water temperatures in parts of the equatorial Pacific, made its return in June 2026. Observations of sea surface height from the Sentinel-6 Michael Freilich satellite that month ...

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. ...

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