File:Drivers of hypoxia and acidification in upwelling shelf systems.svg

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current18:37, 30 November 2022Thumbnail for version as of 18:37, 30 November 2022429 × 348 (635 KB)commons>Mikhail Ryazanov=={{int:filedesc}}== {{Information |description={{en|1=Drivers of hypoxia and ocean acidification intensification in upwelling shelf systems. Equatorward winds drive the upwelling of low dissolved oxygen (DO), high nutrient, and high dissolved inorganic carbon (DIC) water from above the oxygen minimum zone. Cross-shelf gradients in productivity and bottom water residence times drive the strength of DO (DIC) decrease (increase) as water transits across a productive continental shelf. Variation...

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