Previous estimation suggested a steadily strengthening global ocean carbon sink since 2001, after a weakening in the 1990s. However, the increases of carbon sink were asynchronous in different research. Here we reestimated the global ocean carbon sink during 1992-2020 using a new stepwise FFNN pCO2 product. Although the ocean is the sink of atmospheric CO2 in general, the global ocean carbon sink repeatedly strengthened and weakened in the last thirty years, which dominantly caused by the variability of Pacific Ocean carbon sink driven by the ENSO events. The Eastern equatorial Pacific may release more CO2 to the atmosphere because of the strengthened upwelling during the La Nina in the last thirty years. In addition, the reestimated carbon sink of the Southern Ocean has not been increasing as previous research. The SOCAT data used to construct Southern Ocean pCO2 are far more observed in summer than in winter, which underestimates the carbon source intensity of the Southern Ocean in winter in previous research. Although the ocean carbon sink is not always strengthening with the increase of atmospheric CO2 concentration, but the global ocean carbon sinks have been increasing since 2008, reaching 2.14±0.33 Pg C yr-1 in 2020.