Seasonal Phase Relationships between Sea Surface Salinity, Surface Freshwater Forcing, and Ocean Surface Processes
Frederick M. Bingham | Susannah Brodnitz
Sea surface salinity (SSS) can change as a result of surface freshwater forcing (FWF) or internal ocean processes such as upwelling or advection. SSS should follow FWF by ¼ cycle, or 3 months, if FWF is the primary process controlling it at the seasonal scale. In this paper, we compare the phase relationship between SSS and FWF (i.e., evaporation minus precipitation over mixed layer depth) over the global (non-Arctic) ocean using in situ SSS and satellite evaporation and precipitation. We found that, instead of the expected 3-month delay between SSS and FWF, the delay is mostly closer to 1–2 months, with SSS peaking too soon relative to FWF. We then computed monthly vertical entrainment and horizontal advection terms of the upper ocean salinity balance equation and added their contributions to the phase of the FWF. The addition of these processes to the seasonal upper ocean salinity balance leads to the phase difference between SSS and the forcing processes being closer to the expected value. We conducted a similar computation with the amplitude of the seasonal SSS and the forcing terms, with less definitive results. The results of this study highlight the important role that ocean processes play in the global freshwater cycle at the seasonal scale.
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