Surface ocean pH variations since 1689 CE and recent ocean acidification in the tropical South Pacific View Full Text


Ontology type: schema:ScholarlyArticle      Open Access: True


Article Info

DATE

2018-12

AUTHORS

Henry C. Wu, Delphine Dissard, Eric Douville, Dominique Blamart, Louise Bordier, Aline Tribollet, Florence Le Cornec, Edwige Pons-Branchu, Arnaud Dapoigny, Claire E. Lazareth

ABSTRACT

Increasing atmospheric CO2 from man-made climate change is reducing surface ocean pH. Due to limited instrumental measurements and historical pH records in the world's oceans, seawater pH variability at the decadal and centennial scale remains largely unknown and requires documentation. Here we present evidence of striking secular trends of decreasing pH since the late nineteenth century with pronounced interannual to decadal-interdecadal pH variability in the South Pacific Ocean from 1689 to 2011 CE. High-amplitude oceanic pH changes, likely related to atmospheric CO2 uptake and seawater dissolved inorganic carbon fluctuations, reveal a coupled relationship to sea surface temperature variations and highlight the marked influence of El Niño/Southern Oscillation and Interdecadal Pacific Oscillation. We suggest changing surface winds strength and zonal advection processes as the main drivers responsible for regional pH variability up to 1881 CE, followed by the prominent role of anthropogenic CO2 in accelerating the process of ocean acidification. More... »

PAGES

2543

References to SciGraph publications

Identifiers

URI

http://scigraph.springernature.com/pub.10.1038/s41467-018-04922-1

DOI

http://dx.doi.org/10.1038/s41467-018-04922-1

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1105107301

PUBMED

https://www.ncbi.nlm.nih.gov/pubmed/29959313


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