The Longfengtou Beach in the Haitan Bay,located in Fujian Province of China and facing the Haitan Strait,has been suffering severe erosion due to the construction of seawalls.A simple beach nourishment project implemented has not achieved the anticipated beach restoration.Thus a practical solution has to rely on a combination with near-shore marine structures.In this study,a 2-D calibrated flow model is set up to investigate the effects of three different layouts of near-shore marine structures on the tidal current.It is shown that the breakwaters situated in both the north and south ends play a vital part in the protection against erosion.The offshore breakwaters can serve as a barrier to obstruct the current circulation then reduce the current velocity.The groyne linking the Guimo islet and the coast significantly reduces the south-to-north water exchange through the channel and redirects the current direction nearly perpendicular to the north breakwater,which cuts off the longshore transport that may have a negative influence on the beach,especially,the northern part.It is also noted that the monsoon at the site with different directions increases the current velocity.In general,proper layouts of marine structures can reduce the current velocity thus lead to less intense sand transport near the beach. The Longfengtou Beach in the Haitan Bay, located in Fujian Province of China and facing the Haitan Strait, has been suffering severe erosion due to the construction of seawalls. A simple beach nourishment project implemented has not achieved the expected beach restoration. Touh a practical solution has to rely on a combination with near-shore marine structures. In this study, a 2-D calibrated flow model is set up to investigate the effects of three different layouts of near-shore marine structures on the tidal current. It is shown that the breakwaters situated in both the north and south ends play a vital part in the protection of erosion. the offshore breakwaters can serve as a barrier to obstruct the current; then reduce the current velocity. the groyne linking the Guimo islet and the can significantly the south-to-north water exchange through the channel and redirects the current direction nearly perpendicular to the north breakwater, which cuts off the longshore transport that may have a negative influence on the beach, especially, the northern part.It is also noted that the monsoon at the site with different directions increases the current velocity.In general, proper layouts of marine structures can reduce the current velocity thus lead to less intense sand transport near the beach.