Articles

This study investigates the spatial and temporal dynamics of shoreline deformation along the San Bartholomeo River over 30 years (1995–2025) using an integrated geospatial approach. The research combines Interferometric Synthetic Aperture Radar (InSAR) and Digital Shoreline Analysis System (DSAS) techniques to quantify both vertical land motion and horizontal shoreline change. Results reveal a decline in land area from 32.622 km² (56.65%) in 1995 to 30.284 km² (52.59%) in 2025, alongside an increase in water body extent, indicating progressive shoreline retreat. Shoreline change rates varied significantly, with erosion reaching −8.04 m/yr and accretion up to 16.73 m/yr. Net Shoreline Movement (NSM) and Shoreline Change Envelope (SCE) analyses further highlighted zones of persistent erosion and high variability. InSAR-derived deformation patterns confirmed the presence of subsidence contributing to shoreline instability. The findings demonstrate that a combination of hydrodynamic forces, sediment imbalance, and anthropogenic activities drives shoreline deformation in the study area. This study contributes to improved shoreline monitoring by integrating vertical and horizontal deformation metrics, providing a robust framework for sustainable shoreline management in deltaic environments.