Articles | Volume 15, issue 18
https://doi.org/10.5194/bg-15-5653-2018
https://doi.org/10.5194/bg-15-5653-2018
Research article
 | 
21 Sep 2018
Research article |  | 21 Sep 2018

Increase of dissolved inorganic carbon and decrease in pH in near-surface waters in the Mediterranean Sea during the past two decades

Liliane Merlivat, Jacqueline Boutin, David Antoine, Laurence Beaumont, Melek Golbol, and Vincenzo Vellucci

Viewed

Total article views: 3,460 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,256 1,118 86 3,460 75 80
  • HTML: 2,256
  • PDF: 1,118
  • XML: 86
  • Total: 3,460
  • BibTeX: 75
  • EndNote: 80
Views and downloads (calculated since 06 Jul 2017)
Cumulative views and downloads (calculated since 06 Jul 2017)

Viewed (geographical distribution)

Total article views: 3,460 (including HTML, PDF, and XML) Thereof 3,306 with geography defined and 154 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 15 Nov 2024
Short summary
The fugacity of carbon dioxide in seawater (fCO2) was measured hourly in the surface waters of the NW Mediterranean Sea during two 3-year sequences separated by 18 years. A decrease of pH of 0.0022 yr−1 was computed. About 85 % of the accumulation of dissolved inorganic carbon (DIC) comes from chemical equilibration with increasing atmospheric CO2; the remaining 15 % accumulation is consistent with estimates of transfer of Atlantic waters through the Gibraltar Strait.
Altmetrics
Final-revised paper
Preprint