{"refrec":{"BRefID":365298,"RR":"<b>Landschützer, P.</b> (2023). CO<sub>2</sub> in the surface ocean. <i>Oxford research encyclopedias: climate science 21 June</i>: 1-31. <a href=\"https://dx.doi.org/10.1093/acrefore/9780190228620.013.885\" target=\"_blank\">https://dx.doi.org/10.1093/acrefore/9780190228620.013.885</a>","BEntID":363018,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". <i>Oxford research encyclopedias: climate science 21 June</i>: 1-31. <a href=\"https://dx.doi.org/10.1093/acrefore/9780190228620.013.885\" target=\"_blank\">https://dx.doi.org/10.1093/acrefore/9780190228620.013.885</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Landschützer, P.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Landschützer, P.","Englishabstract":"The global ocean comprises a significant sink for human-emitted carbon dioxide, yet many different processes are at play, causing strong spatial and temporal variations in the distribution of the sea surface pCO<sub>2</sub> and the resulting air-sea CO<sub>2</sub> fluxes. While dominated by the temperature-driven solubility, physical transport and biogeochemistry, the increase in the sea surface CO<sub>2</sub> partial pressure over the past decades is closely following the increase in atmospheric CO<sub>2</sub>, resulting in a decreasing pH and decreasing saturation states of calcite and aragonite minerals. 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