In recent years, global warming due to an increase in atmospheric CO
2 concentrations is the most urgent concern for maintaining sustainable development in the future. The ocean is one of the most important reservoirs, acting as a sink for the increasing atmospheric CO
2. However, there remain considerable uncertainties in estimates of the oceanic CO
2 uptake. In the western North Pacific, the Japan Meteorological Agency has periodically conduted on board observations of oceanic CO
2 and hydrographic properties from 3° N to 34° N along 137° E every winter since the early 1980s. The 26-year observation records exhibited increasing long-term trends of oceanic CO
2 with similar growth rates to those of atmospheric CO
2 in the extensive subtropical to equatorial zones, suggesting a persistent invasion of anthropogenic CO
2 into the ocean from the atmosphere. The recent uptake of anthropogenic carbon by the ocean has given rise to changes in the chemical equilibrium of the surface ocean CO
2 system, resulting in a reduction of seawater pH, i.e., ocean acidification. It is important to fully understand the mechanisms of the changes in the carbonate system responding to the climate shift for future predictions of the role of the western North Pacific in global carbon cycles.
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