A climate/OA/SRM link?

Greg

Tropical cyclones cause CaCO3 undersaturation of coral reef seawater in a 
high-CO2 
world<http://feedproxy.google.com/~r/wordpress/lRgb/~3/G8ZcIxq3gts/?utm_source=feedburner&utm_medium=email>

Posted: 09 Sep 2013 12:56 AM PDT

Ocean acidification is the global decline in seawater pH and calcium carbonate 
(CaCO3) saturation state (Ω) due to the uptake of anthropogenic CO2 by the 
world’s oceans. Acidification impairs CaCO3 shell and skeleton construction by 
marine organisms. Coral reefs are particularly vulnerable, as they are 
constructed by the CaCO3 skeletons of corals and other calcifiers. We 
understand relatively little about how coral reefs will respond to ocean 
acidification in combination with other disturbances, such as tropical 
cyclones. Seawater carbonate chemistry data collected from two reefs in the 
Florida Keys before, during, and after Tropical Storm Isaac provide the most 
thorough data to-date on how tropical cyclones affect the seawater CO2-system 
of coral reefs. Tropical Storm Isaac caused both an immediate and prolonged 
decline in seawater pH. Aragonite saturation state was depressed by 1.0 for a 
full week after the storm impact. Based on current ‘business-as-usual’ CO2 
emissions scenarios, we show that tropical cyclones with high rainfall and 
runoff can cause periods of undersaturation (Ω < 1.0) for high-Mg calcite and 
aragonite mineral phases at acidification levels before the end of this 
century. Week-long periods of undersaturation occur for 18 mol% high-Mg calcite 
after storms by the end of the century. In a high-CO2 world, CaCO3 
undersaturation of coral reef seawater will occur as a result of even modest 
tropical cyclones. The expected increase in the strength, frequency, and 
rainfall of the most severe tropical cyclones with climate change in 
combination with ocean acidification will negatively impact the structural 
persistence of coral reefs over this century.

Manzello D., Enochs I., Musielewicz S., Carlton R. & Gledhill D., in press. 
Tropical cyclones cause CaCO3 undersaturation of coral reef seawater in a 
high-CO2 world. Journal of Geophysical Research: Oceans.

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