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The abandoned large tributary channel continues to migrate until it is completely filled up with sediments.
Measured sedimentation rate in the abandoned large tributary channel reaches up to 20 cm/month.
Simple and compound dunes are developed on the intertidal tributary channel and channel bank of Yeochari macrotidal flat in the northern Gyeonggi Bay, west coast of Korea.
The dilution mixing model is widely used for this purpose in tributary channel systems that transport contaminants as bed-material load without significant overbank sedimentation.
The channel-migration rate also varies with elevation and location, being greatest in the upper intertidal zone and at the large tributary channel, respectively.
Three-year morphodynamic observations revealed that simple dunes on the tributary channel migrate seaward as fast as 1.5 2 m per day.
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The channels are classified into three size categories, i.e., main channels, large tributary channels and small tributary channels.
Debris flows occurred on steep hillslopes and tributary channels in the most intensely burned areas.
Large tributary channels are 100 150 m wide and up to 3 m deep at bankful stage.
The width and depth of small tributary channels are smaller than 10 m and 1.5 m, respectively.
Its narrow, deep tributary channels extend almost to the Jotunheim Mountains on the east and to the Jostedals Glacier on the north.
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