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The primary downstream consequences of dams are sediment transport and the balance between channel sedimentation and erosion. The distribution of flow velocities is altered, and river channels are cut, as a result of silt entrapment by dams and reservoirs.
Flooding in the downstream is frequently brought on by prolonged, powerful storms. Runoff made of saturated solids is produced by the additional water.
Upstream flooding is more likely if the exceedance flow cannot discharge freely due to the downstream system. For instance, when releasing into coastal locations, tide levels may impact how well surface flood channels work. The primary downstream consequences of dams are sediment transport and the balance between channel sedimentation and erosion. The distribution of flow velocities is altered, and river channels are cut, as a result of silt entrapment by dams and reservoirs.
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