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Figure 1: Principle change in a flood wave due to temporary flood water storage

Figure 1: Principle change in a flood wave due to intermediate storage. If water is retained in the area because the river has room to spread out, the flood wave is less steep. However, the discharge rate remains constant (hatched areas are the same size). Figure according to the Bavarian State Office for the Environment.

If water is retained in the area because the river has room to spread out, the flood wave is less steep. However, the discharge rate remains constant (hatched areas are the same size). Figure according to the Bavarian State Office for the Environment.

Source: Matthias Rothe / UBA
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