TY - JOUR
T1 - Ocean circulation and biogeochemistry moderate interannual and decadal surface water pH changes in the Sargasso Sea
AU - Goodkin, Nathalie F.
AU - Wang, Bo Shian
AU - You, Chen Feng
AU - Hughen, Konrad A.
AU - Grumet-Prouty, Nancy
AU - Bates, Nicholas R.
AU - Doney, Scott C.
N1 - Publisher Copyright:
© 2015. The Authors.
PY - 2015/6/28
Y1 - 2015/6/28
N2 - The oceans absorb anthropogenic CO2 from the atmosphere, lowering surface ocean pH, a concern for calcifying marine organisms. The impact of ocean acidification is challenging to predict as each species appears to respond differently and because our knowledge of natural changes to ocean pH is limited in both time and space. Here we reconstruct 222 years of biennial seawater pH variability in the Sargasso Sea from a brain coral, Diploria labyrinthiformis. Using hydrographic data from the Bermuda Atlantic Time-series Study and the coral-derived pH record, we are able to differentiate pH changes due to surface temperature versus those from ocean circulation and biogeochemical changes. We find that ocean pH does not simply reflect atmospheric CO2 trends but rather that circulation/biogeochemical changes account for >90% of pH variability in the Sargasso Sea and more variability in the last century than would be predicted from anthropogenic uptake of CO2 alone.
AB - The oceans absorb anthropogenic CO2 from the atmosphere, lowering surface ocean pH, a concern for calcifying marine organisms. The impact of ocean acidification is challenging to predict as each species appears to respond differently and because our knowledge of natural changes to ocean pH is limited in both time and space. Here we reconstruct 222 years of biennial seawater pH variability in the Sargasso Sea from a brain coral, Diploria labyrinthiformis. Using hydrographic data from the Bermuda Atlantic Time-series Study and the coral-derived pH record, we are able to differentiate pH changes due to surface temperature versus those from ocean circulation and biogeochemical changes. We find that ocean pH does not simply reflect atmospheric CO2 trends but rather that circulation/biogeochemical changes account for >90% of pH variability in the Sargasso Sea and more variability in the last century than would be predicted from anthropogenic uptake of CO2 alone.
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U2 - 10.1002/2015GL064431
DO - 10.1002/2015GL064431
M3 - Article
AN - SCOPUS:84948712978
SN - 0094-8276
VL - 42
SP - 4931
EP - 4939
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 12
ER -