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Substantial Inter-Model Variation in Oae Efficiency Between the CESM2/Marbl and Ecco-Darwin Ocean Biogeochemistry Models
Induction of a CO2 partial pressure (pCO2) deficit in the surface-ocean through ocean alkalinity enhancement (OAE) or direct ocean removal (DOR) methods has been recognized as a promising approach to meet the projected need for negative CO2 emissions. The difficulty of directly measuring the counter
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