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Drivers of hypoxia and acidification in upwelling shelf systems
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Description
English: 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. Variations in source water DO, DIC, and nutrient content, upwelling favorable winds, and shelf processes can all accentuate or dampen the severity of hypoxia and OA exposure.

Modified from Gewin (2010) by Moni Kovacs.

  • Gewin, V. (2010) "Oceanography: Dead in the water". Nature, 466(7308): 812. doi:10.1038/466812a.
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https://tos.org/oceanography/article/the-dynamics-and-impact-of-ocean-acidification-and-hypoxia

doi:10.5670/oceanog.2019.312
Author Francis Chan, John A. Barth, Kristy J. Kroeker, Jane Lubchenco and Bruce A. Menge. Modified from Gewin (2010) by Moni Kovacs.

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current05:21, 8 July 2020Thumbnail for version as of 05:21, 8 July 20201,433 × 1,163 (497 KB)Epipelagic (talk | contribs)Uploaded a work by Francis Chan, John A. Barth, Kristy J. Kroeker, Jane Lubchenco and Bruce A. Menge. Modified from Gewin (2011) by Moni Kovacs from https://tos.org/oceanography/article/the-dynamics-and-impact-of-ocean-acidification-and-hypoxia {{doi|10.5670/oceanog.2019.312}} with UploadWizard

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