S´
wina Gate Sandspit (Fig. 6, profiles 4, 5). Aeolian
accumulation on the beach has the highest efficiency
when the wind is oblique to the beach/dune (e.g. Arens,
1994). On the investigated area, the heaviest winds are
oblique for part of coast exposed on NW and NE
directions – outside of coastal part on the Uznam
Island, western and eastern part of middle part of
sandspit on the Wolin Island. That is why, new dune
development and the biggest embryo dunes covered by
dense grass carpet are observed. This is the visible sign
of aeolian accumulation on the beach.