Abstract
Multi-decadal trends of the total dissolved inorganic carbon (DIC) concentrations and consequent ocean acidification in surface seawater were investigated on the basis of data from shipboard measurements conducted since 1996 along the 165°E repeat line in the western North Pacific. The observed trends exhibited clear meridional variabilities, with higher rates in the subtropical and tropical zones and lower rates in the subarctic zone, with a DIC range from +0.09 ± 0.14 to +1.64 ± 0.16 μmol kg−1 yr−1 and pH range from −0.0023 ± 0.0034 to −0.0281 ± 0.0059 decade−1. DIC and acidification trends were consistent with those expected from the atmospheric CO2 concentrations at nearly all latitudinal zones, but were significantly different at some latitudes. We attribute the significantly lower rates observed in the central western Subarctic Gyre and southern Subtropical Gyres primarily to the variabilities in upward DIC supply from the subsurface associated with the variability in ocean circulation. However, the higher rate observed to the south of the Kuroshio Extension appears to have been caused by the change in winter vertical mixing related to the change in its stable/unstable paths.
Key Points
- Meridional variability was found in the trends of dissolved inorganic carbon in the surface layer along the 165°E repeat line
- Extremely slow rates of increase observed in the subarctic and tropics are attributed to ocean circulation variability
- A fast increase in the south of the Kuroshio Extension is likely associated with the variability in its path
Ono H., Toyama K., Enyo K., Iida Y., Sasano D., Nakaoka S.-I. & Ishii M., 2023. Meridional variability in multi-decadal trends of dissolved inorganic carbon in surface seawater of the western North Pacific along the 165°E line. Journal of Geophysical Research: Oceans 128: e2022JC018842. doi: 10.1029/2022JC018842. Article.
