Collapse of the tropical and subtropical North Atlantic CO(2) sink in boreal spring of 2010

Following the 2009 Pacific El Niño, a warm event developed in the tropical and subtropical North Atlantic during boreal spring of 2010 promoted a significant increase in the CO(2) fugacity of surface waters. This, together with the relaxation of the prevailing wind fields, resulted in the reversal o...

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Detalles Bibliográficos
Autores principales: Ibánhez, J. Severino P., Flores, Manuel, Lefèvre, Nathalie
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5278357/
https://www.ncbi.nlm.nih.gov/pubmed/28134309
http://dx.doi.org/10.1038/srep41694

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5278357/
https://www.ncbi.nlm.nih.gov/pubmed/28134309
http://dx.doi.org/10.1038/srep41694

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