“…As the tidal range of the South-Eastern Baltic coasts is not significant and barely reaches 3.5-4.0 cm [44,45], the wind-generated waves [46], the prevailing alongshore currents, and accordingly the sand transport from south to north [35,[47][48][49] and the aeolian processes [42] are the main beachforming factors on the Lithuanian Baltic Sea coast. The most significant short-term sea level As the tidal range of the South-Eastern Baltic coasts is not significant and barely reaches 3.5-4.0 cm [44,45], the wind-generated waves [46], the prevailing alongshore currents, and accordingly the sand transport from south to north [35,[47][48][49] and the aeolian processes [42] are the main beach-forming factors on the Lithuanian Baltic Sea coast. The most significant short-term sea level fluctuations near the Lithuanian coast occur due to storm surges.…”