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<identifier>oai:HAL:hal-01286093v1</identifier>
<datestamp>2016-03-11</datestamp>
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<publisher>HAL CCSD</publisher>
<title lang=en>Time variability of the north-western Mediterranean Sea pH over 1995–2011</title>
<creator>Marcellin Yao, Koffi</creator>
<creator>Marcou, Olivier</creator>
<creator>Goyet, Catherine</creator>
<creator>Guglielmi, Véronique</creator>
<creator>Touratier, Franck</creator>
<creator>Savy, Jean-Philippe</creator>
<contributor>Centre de Recherches Océanologiques (CRO)</contributor>
<contributor>Institut de Modélisation et d'Analyses en Géo-Environnement et Santé - Espace Développement (IMAGES-Espace DEV) ; Université de Perpignan Via Domitia (UPVD) - Espace pour le Développement (UMR ESPACE-DEV) ; Université des Antilles et de la Guyane (UAG) - Université de la Réunion - Université de Montpellier (UM) - Institut de Recherche pour le Développement (IRD) - Université des Antilles et de la Guyane (UAG) - Université de la Réunion - Université de Montpellier (UM) - Institut de Recherche pour le Développement (IRD)</contributor>
<description>International audience</description>
<source>ISSN: 0141-1136</source>
<source>Marine Environmental Research</source>
<publisher>Elsevier</publisher>
<identifier>hal-01286093</identifier>
<identifier>https://hal-univ-perp.archives-ouvertes.fr/hal-01286093</identifier>
<source>https://hal-univ-perp.archives-ouvertes.fr/hal-01286093</source>
<source>Marine Environmental Research, Elsevier, 2016, <10.1016/j.marenvres.2016.02.016></source>
<identifier>DOI : 10.1016/j.marenvres.2016.02.016</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.marenvres.2016.02.016</relation>
<language>en</language>
<subject lang=en>Ocean acidification</subject>
<subject lang=en>Anthropogenic CO2</subject>
<subject lang=en>Mediterranean sea</subject>
<subject>[SDU.STU.OC] Sciences of the Universe [physics]/Earth Sciences/Oceanography</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>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.</description>
<date>2016-03</date>
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