The advent of L-band passive microwave remote sensing in the last decade (2010 to present) has allowed for the first time the retrieval of global high-resolution sea surface salinity (SSS) from space (Reul et al., 2014;Vinogradova et al., 2019). These new SSS datasets have opened the modern era of salinity science, leading to new insights into the role of salinity in ocean circulation, water mass formation, the water cycle, and climate variability and change (Reul et al., 2020). Like many typical time series, the most characteristic signal of satellite SSS is the seasonal cycle, a pattern that is repetitive from year to year and has variability generally greater than intraseasonal, interannual, and longer-timescale variability (Bingham & Lee, 2017;Dinnat et al., 2019). To facilitate the detection of climate-induced fluctuations that have smaller magnitudes, the