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The tropical Pacific is the largest source region of CO2 release to the atmosphere through the sea surface, with air–sea CO2 fluxes varying on seasonal to interdecadal timescales, which is attributed to several factors. At present, there is no consensus on the relative contributions of wind speed and ΔpCO2 (the partial pressure of CO2 [pCO2] difference between sea surface and the atmosphere) to the...
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