What is it about?
It tries to fully explain the effect of physical, biological and chemical processes on sea surface pCO2 dynamics in an important ocean margin.
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Why is it important?
It is the first time to clearly explain the effect of chemical buffering capacity on sea surface pCO2 dynamics.
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This page is a summary of: Spring carbonate chemistry dynamics of surface waters in the northern East China Sea: Water mixing, biological uptake of CO2, and chemical buffering capacity, Journal of Geophysical Research Oceans, September 2014, American Geophysical Union (AGU),
DOI: 10.1002/2014jc009856.
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