The Stokes-drift have an effect that cannot be ignored on flow field and temperature field structure on the ocean mixed layer. This paper used the wave simulation results based on WAVEWATCHⅢ model to calculate Stokes-drift and introduced it into SBPOM mode in the momentum equation. From the perspective of volume transport, we studied the impact of Stokes-drift on the global sea surface temperature. The results show that spatial distribution of Stokes-drift and Stokes transport in the world present a zonal distribution characteristics that high latitude is larger and the flow and transport has a cooling effect on the global sea surface temperature. The cooling effect distribution is corresponding to the intensity of global Stokes transport and the cooling effect in high latitudes is greater than the middle and low. Especially in the Antarctic Circumpolar Current, average cooling effect is significantly greater than the rest of the waters. The largest cooling can reach 1.5 ℃ and the global average cooling is ove 0.1 ℃.