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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...
Autores principales: | , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group
2016
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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 |