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Decadal acidification in Atlantic and Mediterranean water masses exchanging at the Strait of Gibraltar
Seawater pH is undergoing a decreasing trend due to the absorption of atmospheric CO(2), a phenomenon known as ocean acidification (OA). Biogeochemical processes occurring naturally in the ocean also change pH and hence, for an accurate assessment of OA, the contribution of the natural component to...
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| Pubblicato in: | Sci Rep |
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| Autori principali: | , , , , |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
Nature Publishing Group UK
2019
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| Soggetti: | |
| Accesso online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6820531/ https://ncbi.nlm.nih.gov/pubmed/31664139 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-019-52084-x |
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