Time variability of the north-western Mediterranean Sea pH over 1995-2011

Mar Environ Res. 2016 May:116:51-60. doi: 10.1016/j.marenvres.2016.02.016. Epub 2016 Mar 4.

Abstract

Factors controlling ocean acidification and its temporal variations were studied over the 1995-2011 period at the Dyfamed site at 10 m depth, in the North Mediterranean Sea. The results indicated a mean annual decrease of 0.003 ± 0.001 pH units on the seawater scale. The seasonal variability was characterized by a pH decrease during springtime and a strong pH increase in late fall. Anthropogenic CO2 (CANT) absorption by the ocean was the key driver of seawater acidification in this region, accounting for about 70% of the observed drop in pH, followed by water temperature (about 30%). The total inorganic carbon (CT) data showed a CT increase of 30.0 ± 1.0 μmol kg(-1) per decade. This decadal increase is mainly due to the CANT penetration (43.2 μmol kg(-1) per decade) in surface waters, which is mitigated for by relatively small opposing changes in CT due to physical and biological processes.

Keywords: Anthropogenic CO(2); Mediterranean sea; Ocean acidification.

Publication types

  • Research Support, Non-U.S. Gov't

MeSH terms

  • Carbon Dioxide / metabolism
  • Environmental Monitoring*
  • Hydrogen-Ion Concentration
  • Mediterranean Sea
  • Seasons*
  • Seawater / chemistry*
  • Temperature
  • Time Factors

Substances

  • Carbon Dioxide