“…Coastal SWH observations from satellite altimetry are often discarded or are of bad quality due to coastal interference that originates from strongly reflective targets such as sandbanks, sheltered bays, or calm waters close to the shoreline. Schlembach et al (2022) showed that the correlation of SWH data of the operational baseline product of S3 with in-situ data from buoys amounts to less than 0.20 for closer than 20 km from the coast. Tailored retracking algorithms have been developed to account for the coastal interference, such as ALES (Passaro et al, 2015), Brown-Peaky (Peng and Deng, 2018) for the conventional low resolution mode (LRM) altimetry, and SAMOSA+ (Dinardo et al, 2018), SAMOSA++ (Dinardo et al, 2020), ALES + SAR (Passaro et al, 2021), RiwiSAR-SWH (Gou and Tourian, 2021), CORS (Garcia et al, 2022), or CORALv1 (Schlembach et al, 2022) for UF-SAR altimetry.…”