Water level and height of flood line.* The points where the flood line is lower than the other points may underestimate the actual high-water levels because the values were determined based on evidence from plants, such as damage to the grass. Using ArcGIS, we calculated based on the topography, water depth, and area of the retarding basin that 378,203.0 m 3 of floodwater was stored on the flood plain in Okawano at the time of the maximum water level of 19.05 m, demonstrating that the open levee reduced the downstream flood volume. Rice had been planted in the paddy fields in the retarding basin, but except for a very small area near the inlet, the plants survived. There was little debris influx, driftwood, or mud deposition, and there was no significant damage to the paddy fields (Figure 6).

Water level and height of flood line.* The points where the flood line is lower than the other points may underestimate the actual high-water levels because the values were determined based on evidence from plants, such as damage to the grass. Using ArcGIS, we calculated based on the topography, water depth, and area of the retarding basin that 378,203.0 m 3 of floodwater was stored on the flood plain in Okawano at the time of the maximum water level of 19.05 m, demonstrating that the open levee reduced the downstream flood volume. Rice had been planted in the paddy fields in the retarding basin, but except for a very small area near the inlet, the plants survived. There was little debris influx, driftwood, or mud deposition, and there was no significant damage to the paddy fields (Figure 6).

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Large-scale disasters, such as hurricanes, cyclones, tsunamis, and forest fires, have caused considerable damage in recent years. This study investigated two case studies of discontinuous open levees (kasumi-tei), which are a traditional Japanese river technology, on the Matsuura River at the sites of Okawano and Azame-no-se, and evaluated the adva...

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... status at the time of flood event [27,34]. It is concluded by examining the flood lines in Figure 5 that the lines are concentrated near an elevation of 19 m at each location within the retarding basin of the Oka-wano open levee system. In other words, within the retarding basin, the height of the water surface was almost constant, regardless of the distance from the inlet. ...

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