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Morphology of sand spit at a river mouth is afEected by combined forces, such as tidal current, sea waves and river discharge, etc. Topographical change at a river mouth can beremarkable dependent on time-variation of these forces. However, in order to obtain frequent topography data at a river mouth, it is necessary to consume a great amount of time and cost, Thus, if it is possible to estimate river mouth topography information from water level variation data, it will bepractically efEective for river mouth management. However, river mouth characteristic sdiferent in each river. Therefore, it is necessary to clarify the river mouthch aracteristics. In thisstudy, water depth estimation method is applied to field ata at a river mouth. Moreover, the application limit of this method was discussed

Estinlation Method of Water Depth at the River Mouth and Limit of Application