A regional ocean biogeochemical model for the Bering Sea is used to dynamically
downscale three Earth System Models from the CMIP5 archive under the RCP 8.5 and RCP …

The Bering Sea is highly vulnerable to ocean acidification (OA) due to naturally cold, poorly
buffered waters and ocean mixing processes. Harsh weather conditions within this rapidly …

The continental shelves of the Pacific-Arctic Region (PAR) are especially vulnerable to the
effects of ocean acidification (OA) because the intrusion of anthropogenic CO₂ is not the …

Ocean acidification (OA) is increasing predictably in the global ocean as rising levels of
atmospheric carbon dioxide lead to higher oceanic concentrations of inorganic carbon. The …

The coastal ecosystem of the Gulf of Alaska (GOA) is especially vulnerable to the effects of
ocean acidification and climate change. Detection of these long-term trends requires a good …

Climate change impacts coastal ecosystems through large scale changes in temperature,
stratification, circulation and ocean acidification. Here, the potential response of the British …

Ocean acidification (OA) results in reduced seawater pH and aragonite saturation state
(Ωarag), but also reduced seawater buffer capacity. As buffer capacity decreases, diel …

Ocean acidification (OA) is often defined as the gradual decline in pH and aragonite
saturation state (ΩAr) for open ocean waters as a result of increasing atmospheric pCO2 …

Due to seasonal upwelling, the upper ocean waters of the California Current System (CCS)
have a naturally low pH and aragonite saturation state (Ω arag), making this region …

We reconstruct the evolution of ocean acidification in the California Current System (CalCS)
from 1979 through 2012 using hindcast simulations with an eddy-resolving ocean …