Sea surface temperature (SST) is a key parameter used in physical ocean research and has an important influence on sea-air interaction and global climate change. Space-borne microwave and infrared radiometers are the main methods used in SST remote sensing. However, although microwave radiometers provide all-weather technology their spatial resolution is sparse, and although infrared radiometers have a good resolution they are affected by cloud. In this study, a 0.1° daily SST fusion product is analyzed using the optimum interpolation method. Data resources include WindSat, AMSR-E, ASMR2, HY-2 RM, MODIS, and AVHRR. Buoy data are used to validate and correct the fusion SST product and its SST characteristics in the Bohai and the Huanghai Seas are also studied. Results show that the RMS error of this SST product is 1.1℃, but this decreases slightly after correction. SST characteristics show the lowest standard deviation of SST is in winter, and SST tends to be inhomogeneous in spring when sea temperatures rise.