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Disparate acidification and calcium carbonate desaturation of deep and shallow waters of the Arctic Ocean

The Arctic Ocean is acidifying from absorption of man-made CO(2). Current predictive models of that acidification focus on surface waters, and their results argue that deep waters will acidify by downward penetration from the surface. Here we show, with an alternative model, the rapid, near simultan...

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Detalles Bibliográficos
Autores principales: Luo, Yiming, Boudreau, Bernard P., Mucci, Alfonso
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5036158/
https://www.ncbi.nlm.nih.gov/pubmed/27659188
http://dx.doi.org/10.1038/ncomms12821