Cross-Shore Profile Evolution after an Extreme Erosion Event-Palanga, Lithuania

We report cross-shore profile evolution at Palanga, eastern Baltic Sea, where short period waves dominate. Cross-shore profile studies began directly after a significant coastal erosion event caused by storm Anatol, in December of 1999, and continued for a year. Further measurements were undertaken sixteen years later. Cross-shore profile changes were described, and cross-shore transport rates were calculated. A K-means clustering technique was applied to determine sections of the profile with the same development tendencies. Profile evolution was strongly influenced by the depth of closure which is constrained by a moraine layer, and the presence of a groyne. The method used divided the profile into four clusters: the first cluster in the deepest water represents profile evolution limited by the depth of closure, and the second and third are mainly affected by processes induced by wind, wave and water level changes. The most intensive sediment volume changes were observed directly after the coastal erosion event. The largest sand accumulation was in the fourth profile cluster, which includes the upper beach and dunes. Seaward extension of the dune system caused a narrowing of the visible beach, which has led to an increased sand volume (accretion) being misinterpreted as erosion

Automated summary

This study reported the cross-shore profile evolution at Palanga in the eastern Baltic Sea, revealing that the profile changes were influenced by the depth of closure and presence of a groyne. The most significant changes in profile evolution were observed after a coastal erosion event. The results showed that the seaward extension of the dune system led to a narrowing of the visible beach, causing sand accumulation to be misinterpreted as erosion.