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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...
Guardat en:
| Publicat a: | Sci Rep |
|---|---|
| Autors principals: | , , , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Nature Publishing Group UK
2019
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| Matèries: | |
| Accés en línia: | 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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