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- W2165867704 abstract "article i nfo The oceanic uptake of atmospheric carbon dioxide (CO2) since pre-industrial times has increased acidity levels, resulting in a decrease in the pH and aragonite saturation state (Ωar) of surface waters. Aragonite is the predom- inant biogenic form of calcium carbonate precipitated by calcifying organisms in tropical reef ecosystems. Values of Ωar are often used as a proxy for estimating calcification rates in corals and other calcifying species. We quan- tify the regional and seasonal variability of Ωar and its main drivers for the Pacific island region (120°E:140°W, 35°S:30°N). The calculation of Ωar uses a seasonal climatology of the surface-water partial pressure of CO2 ,c om- bined with values of total alkalinity (TA) estimated from a relationship between surface water salinity and total alkalinity that is derived from measurements in the region. This relationship is valid for all phases of El Nino/ Southern Oscillation and for mixed layer waters with less than 15 μmol kg −1" @default.
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- W2165867704 date "2014-04-01" @default.
- W2165867704 modified "2023-09-26" @default.
- W2165867704 title "Seasonal variability of aragonite saturation state in the Western Pacific" @default.
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- W2165867704 doi "https://doi.org/10.1016/j.marchem.2014.01.001" @default.
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