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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Detalles Bibliográficos
Autores principales: Flecha, Susana, Pérez, Fiz F., Murata, Akihiko, Makaoui, Ahmed, Huertas, I. Emma
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6820531/
https://www.ncbi.nlm.nih.gov/pubmed/31664139
http://dx.doi.org/10.1038/s41598-019-52084-x

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6820531/
https://www.ncbi.nlm.nih.gov/pubmed/31664139
http://dx.doi.org/10.1038/s41598-019-52084-x

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