Abstract Sea surface salinity (SSS) is a key indicator of the ocean–atmosphere freshwater balance and plays a central role in global moisture transport. This study investigates how extreme SSS anomalies in the North Atlantic (NATL) source region indicate atmospheric moisture pathways and precipitation in surrounding continental and island sink regions. Monthly SSS data (1985–2014) from the EN4.2.2 data set were combined with high‐resolution Lagrangian moisture tracking via FLEXPART‐WRF simulations. Extreme salinity events (±1 σ , ≥2 consecutive months) were identified and linked to composite anomalies of evaporation, vertically integrated vapor transport and geopotential height. The results show that high‐salinity episodes, driven by prolonged evaporation and anticyclonic regimes, correspond to westward moisture exports to the Caribbean and Central America. In contrast, low‐salinity events coincide with cyclonic anomalies that redirect moisture toward southwestern Europe, notably the Iberian Peninsula and Madeira. Precipitation responses in other island regions were more heterogeneous, reflecting their proximity to the source. A significant lagged correlation with the Oceanic Niño Index suggests ENSO's influence on NATL salinity variability. These findings demonstrate that SSS anomalies can serve as diagnostic indicators of regional hydrological changes, reflecting physical lead‐lag relationships that provide new insights into the variability of moisture transport and its subsequent impact on regional precipitation.
Rosquete‐Estevez et al. (Mon,) studied this question.