Abstract

High swell has been known for the one of the fundamental driver of sea shore disintegration in the east bank of Korea. In this investigation, waterfront geology changes because of high expand is reproduced to discover its impact on the backshore by utilizing portable bed tests and mathematical examinations. Ocean floor geological changes because of different occurrence waves were examined utilizing CSHORE model in the mathematical trials. Moreover, the instrument and the marvels of sea shore disintegration because of waves and high grows on the foreshore and backshore were investigated and contrasted and versatile bed water driven trials. Seaside flooding is a huge and expanding peril. There are different drivers counting rising seaside water levels, more exceptional Hydrologic inputs, shoaling groundwater and urbanization.

Keywords: Coastline; Beach profile; Seaward sediment transport