Oceanic uptake of anthropogenic carbon dioxide (CO 2 ) has acidified open-ocean surface waters by 0.1 pH units since preindustrial times. Despite unequivocal evidence of ocean acidification (OA) via open-ocean measurements for the past several decades, it has yet to be documented in near-shore and coral reef environments. A lack of long-term measurements from these environments restricts our understanding of the natural variability and controls of seawater CO 2 -carbonate chemistry and biogeochemistry, which is essential to make accurate predictions on the effects of future OA on coral reefs. Here, in a 5-y study of the Bermuda coral reef, we show evidence that variations in reef biogeochemical processes drive interannual changes in seawater pH and Ω aragonite that are partly controlled by offshore processes. Rapid acidification events driven by shifts toward increasing net calcification and net heterotrophy were observed during the summers of 2010 and 2011, with the frequency and extent of such events corresponding to increased offshore productivity. These events also coincided with a negative winter North Atlantic Oscillation (NAO) index, which historically has been associated with extensive offshore mixing and greater primary productivity at the Bermuda Atlantic Time-series Study (BATS) site. Our results reveal that coral reefs undergo natural interannual events of rapid acidification due to shifts in reef biogeochemical processes that may be linked to offshore productivity and ultimately controlled by larger-scale climatic and oceanographic processes.O cean acidification (OA) resulting from rising atmospheric CO 2 (1-3) and the associated declines in surface seawater pH and saturation state with respect to CaCO 3 minerals such as aragonite (Ω aragonite = [Ca 2+ ][CO 3 2-]/K sp *, where K sp * is the ion solubility product) have raised concerns on the potential consequences to marine calcifiers and ecosystems (4, 5). Reductions in Ω aragonite have been found to negatively affect organismal CaCO 3 production (6) while accelerating bioerosion and CaCO 3 dissolution (7,8). Hence, it has been hypothesized that coral reefs could shift from a condition of net calcification to net dissolution, with some model estimates predicting a transition for worldwide reefs at atmospheric CO 2 levels of 560 ppm (5, 7).Despite growing concern about the vulnerability of coral reefs, a lack of long-term measurements has prevented direct observation of anthropogenic OA owing to increasing atmospheric CO 2 in these environments. Additionally, short-term observations have revealed large variability and modification of reef seawater CO 2 -carbonate chemistry on diurnal and seasonal timescales as a result of coral reef biogeochemical processes such as photosynthesis, respiration, calcification, and CaCO 3 dissolution (9, 10). It has been hypothesized that these natural processes, quantified as net ecosystem production (NEP = gross primary production − autotrophic and heterotrophic respiration) and net ecosystem calcification (NEC = gro...