Abstract
Saline lakes exhibit complex spectral behaviour due to the coexistence of shallow brine, wet sediments and evaporitic crusts. Instead of a clearly defined shoreline, these environments exhibit hydro-evaporitic transition zones in which surface states vary gradually, producing continuous spectral variations within individual pixels. As a consequence, conventional water and salinity indices often show limited transferability across saline systems with contrasting surface conditions. This study proposes a Sentinel-2 Salinity Water Index (S2SWI) derived from optimised spectral band combinations. Index coefficients were derived using three different approaches: Particle Swarm Optimisation (PSO), Ridge Regression (RR), and a hybrid U-Net + Ridge Regression (UNET+RR) framework. Reference surface classes (water, wet saline margin and crust) were generated through Random Forest classification. The index was developed using three saline lakes within a Leave-One-Lake-Out (LOLO) validation framework to promote spectral formulations that generalize across different environments. Its transferability was subsequently evaluated in three independent lakes by generating S2SWI maps and applying an unsupervised K-means clustering approach; the results were compared with Random Forest (RF) reference classifications. Results indicate that the S2SWI provides a consistent ordering of surface conditions across the six lakes, ranging from liquid hypersaline water to dry evaporitic crusts. Among the three formulations evaluated, the hybrid UNET+RR approach showed the strongest overall transferability, particularly in spectrally challenging systems characterized by extensive transition zones.The proposed S2SWI offers a computationally simple and transferable tool for Sentinel-2 monitoring of saline lakes. Moreover, the comparison between optimization, regression, and hybrid spatial-spectral approaches helps clarify the environmental conditions under which spectral indices remain robust, as well as those in which spatial information can improve the interpretation of surface conditions.

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