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

The British Columbia (BC) shelf along the Pacific coast of Canada is in the transition zone
between coastal upwelling to the south and downwelling to the north. The southern coast is …

Model projections of ocean circulation and biogeochemistry are used to investigate large
scale climate changes under moderate mitigation (RCP 4.5) and high emissions (RCP 8.5) …

One of the major challenges to assessing the impact of ocean acidification on marine life is
detecting and interpreting long-term change in the context of natural variability. This study …

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 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 is a predictable consequence of rising atmospheric carbon dioxide
(CO2), and is highly likely to impact the entire marine ecosystem–from plankton at the base …

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 …

Estuarine systems host a rich diversity of marine life that is vulnerable to changes in ocean
chemistry due to addition of anthropogenic carbon. However, the detection and impact of …

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 …