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Rapid progression of ocean acidification in the California Current System
Gruber, N.; Hauri, C.; Lachkar, Z.; Loher, D.; Frölicher, T.L.; Plattner, G.-K. (2012). Rapid progression of ocean acidification in the California Current System. Science (Wash.) 337(6091): 220-223.
In: Science (Washington). American Association for the Advancement of Science: New York, N.Y. ISSN 0036-8075, more
Peer reviewed article  

Available in  Authors 

    Acidification; Marine

Authors  Top 
  • Gruber, N.
  • Hauri, C.
  • Lachkar, Z.
  • Loher, D.
  • Frölicher, T.L.
  • Plattner, G.-K.

    Nearshore waters of the California Current System (California CS) already have a low carbonate saturation state, making them particularly susceptible to ocean acidification. We used eddy-resolving model simulations to study the potential development of ocean acidification in this system up to the year 2050 under the Special Report on Emissions Scenarios A2 and B1 scenarios. In both scenarios, the saturation state of aragonite Oarag is projected to drop rapidly, with much of the nearshore region developing summer-long undersaturation in the top 60 meters within the next 30 years. By 2050, waters with Oarag above 1.5 will have largely disappeared, and more than half of the waters will be undersaturated year-round. Habitats along the sea floor will become exposed to year-round undersaturation within the next 20 to 30 years. These projected events have potentially major implications for the rich and diverse ecosystem that characterizes the California CS.

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