Prediction of Sea of Japan (East Sea) acidification over the past 40 years using a multiparameter regression model

• Published in: Global Biogeochemical Cycles
• Main Authors: Kim, Tae-Wook, Lee, Kitack, Feely, Richard A., Sabine, Christopher L., Chen, Chen-Tung Arthur, Jeong, Hae Jin, Kim, Kwang Young
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: American Geophysical Union 2022
• Subjects: INCREASED ATMOSPHERIC CO2; FOSSIL-FUEL CO2; OCEAN ACIDIFICATION; ANTHROPOGENIC CO2; DISSOCIATION-CONSTANTS; CARBONIC-ACID; INORGANIC CARBON; ATLANTIC-OCEAN; INDIAN-OCEAN; REDUCED CALCIFICATION; Indian; Carbonic acid; Ocean acidification
• Online Access: https://hdl.handle.net/10371/192743; https://doi.org/10.1029/2009GB003637

A multiparameter linear regression model (MLR) of aragonite saturation state (Omega(ARG)) as a function of temperature, pressure and O-2 concentration in the upper 1,000 m of the Sea of Japan (East Sea) was derived with an uncertainty of +/- 0.020 (1 sigma). The Omega(ARG) data (n = 1,482) used to derive the basin-wide Omega(ARG) prediction model were collected during a field survey in 1999 and were corrected for anthropogenic CO2. Some biases were resolved by addition of a pressure and O-2 concentration interaction term to the proposed model. Correlation between the two predictor terms, caused by addition of this term, was minimized by centering the data for the three variables (thus subtracting the mean from each individual data point). Validation of the model against data sets obtained in 1992 and 2007 yielded correlation coefficients of 0.995 +/- 0.013 for 1992 (n = 64, p << 0.001) and 0.995 +/- 0.009 for 2007 (n = 137, p << 0.001) and root mean square errors of +/- 0.064 for 1992 and +/- 0.050 for 2007. The strong correlation between measurements and predictions suggests that the model can be used to estimate the distribution of Omega(ARG) in the Sea of Japan (East Sea) (including dynamic coastal waters) on varying time scales when basic hydrographic data on temperature, pressure and O-2 concentration are available. Application of the model to past measurements for the Sea of Japan (East Sea) indicated that interdecadal variability (2 sigma from the mean) in Omega(ARG) corrected for anthropogenic CO2 was generally high (0.1-0.7) in the upper water layer (<200 m depth), and decreased (0.05-0.2) with depth for waters deeper than 500 m. The interdecadal variability is largely controlled by variations in the degree of water column ventilation. Superimposed on this natural variability, the input of CO2 derived from fossil fuels has markedly acidified the upper water layers during the anthropocene and thereby moved the aragonite saturation horizon upward by 50-250 m. The impact of CO2 derived from ...