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El reciente aumento de la absorción de carbono oceánico impulsado por la debilidad de la parte superior del océano

Tim DeVries1,2, Mark Holzer3,4, Francois Primeau5

  • 1Department of Geography, University of California, Santa Barbara, California 93106, USA.

Nature
|February 10, 2017
PubMed
Resumen

Los cambios en la circulación oceánica, no las emisiones, están impulsando los cambios en el sumidero de dióxido de carbono (CO2) del océano. El debilitamiento de la circulación en la década de 2000 aumentó la absorción de CO2, pero puede limitar la absorción futura de CO2 antropogénico.

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