Long-term variations in ocean acidification indices in the Northwest Pacific from 1993 to 2018

Long-term variations in ocean acidification indices in the Northwest Pacific were examined using observational data and a biogeochemical model with an operational ocean model product for the period 1993-2018. The model and observational data for the surface ocean (< 100-m depth) exhibit consistent patterns of ocean acidification in the subtropical and Kuroshio Extension regions and relative alkalinization (i.e., reduced acidification) in the subarctic region of the Northwest Pacific. Below 100-m depth, acidification dominated in the subtropical regions and alkalinization in the subarctic regions. We attribute the excess acidification in the subtropical and Kuroshio regions to the vertical mixing of dissolved inorganic carbon (DIC) exceeding the DIC release by air-sea exchange. These regional differences in acidification and alkalinization are attributed to spatially variable biological processes in the upper ocean and horizontal and vertical physical redistribution of DIC. Our model and observational results have implications for the spatial extent and pattern of ocean acidification, along with the strength of the ocean carbon sink, which are key aspects of global climate change.

Automated summary

The study investigated long-term variations in ocean acidification indices in the Northwest Pacific from 1993 to 2018 using observational data and a biogeochemical model. The results showed consistent patterns of acidification in the subtropical and Kuroshio Extension regions, while relative alkalinization was observed in the subarctic region. Regional differences in acidification and alkalinization were attributed to spatially variable biological processes and physical redistribution of DIC.