The tidal flow regime at the shallow sea area is usually decided by topographical factors, such as forms of shorelines, bottom topography, channel, sand bar or tidal flat, etc.
This study is on the Keum River Estuary, which appears exactly phenomeno...
The tidal flow regime at the shallow sea area is usually decided by topographical factors, such as forms of shorelines, bottom topography, channel, sand bar or tidal flat, etc.
This study is on the Keum River Estuary, which appears exactly phenomenons of tide caused by complicated topographical changes, and it is inquired out or not changes of depth and current on numerical experiments before and after constructed Estuary Dike.