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Bathymetric changes around the Tenryu River mouth were analyzed using the narrow-multi beam survey data taken eight times between 2008 and 2010. In 2010 four large floods with a daily discharge greater than 1000 m/s occurred, 4.0 × 10 m of sand was deposited while forming a river mouth terrace immediately offshore of the mouth. In addition, because calm wave condition continued between 2008 and 2010, seabed was eroded in the zone deeper than -6 m, whereas in the zone shallower than -6 m sand was deposited due to the shoreward sand transport, which prevailed under the calm wave conditions.

Field Observation on Response of Topography around Tenryu River Mouth to Floods and Wave Action