资源环境科技发展态势分析平台

The acidification of coastal waters is distinguished from the open ocean because of much stronger synergistic effects between anthropogenic forcing and local biogeochemical processes. However, ocean acidification research is still rather limited in polar coastal oceans. Here, we present a 17-year (2002-2019) observational dataset in the Chukchi Sea to determine the long-term changes in pH and aragonite saturation state (Ω_arag). We found that pH and Ω_arag declined in different water masses with average rates of -0.0047 ± 0.0026 year^-1 and -0.017 ± 0.009 year^-1, respectively, and are ∼2-3 times faster than those solely due to increasing atmospheric CO₂. We attributed the rapid acidification to the increased dissolved inorganic carbon owing to a combination of ice melt-induced increased atmospheric CO₂ invasion and subsurface remineralization induced by a stronger surface biological production as a result of the increased inflow of the nutrient-rich Pacific water.