Flood Routing Process and High Dam Interception of Natural Discharge from the 2018 Baige Landslide-Dammed Lake

The outburst flood of the Baige landslide dam caused tremendous damage to infrastructure, unfinished hydraulic buildings, roads, and bridges that were built or under construction along the Jinsha River. Can downstream hydraulic buildings, such as high dams with flood control and discharge function, accommodate outburst floods or generate more serious losses due to wave overtopping? In this study, the unsteady flow of a one-dimensional hydraulic calculation was used to simulate natural flood discharge. Assuming a high dam (Yebatan arch dam) is constructed downstream, the flood processes were carried out in two forms of high dam interception (complete interception, comprehensive flood control of blocking and draining). Moreover, three-dimensional visualization of the inundation area was performed. Simulation results indicate that the Yebatan Hydropower Station can completely eliminate the outburst flood risk even under the most dangerous situations. This station can reduce the flood peak and delay the peak flood arrival time. Specifically, the flood peak decreased more obviously when it was closer to the upstream area, and the flood peak arrival time was more delayed when the flood spread further downstream. In addition, the downstream water depth was reduced by approximately 10 m, and the inundation area was reduced to half of the natural discharge. This phenomenon shows that hydraulic buildings such as high dams can reduce the inundation area of downstream farmlands and extend the evacuation time for downstream residents during the flood process, thus reducing the loss of life and property.


Introduction
The landslide dam, which is mainly composed of sediment and rock, is weak against water pressure and scouring [1][2][3][4]. When the water depth behind the dam is higher than the highest elevation of the dam, it will destroy the dammed body and form a large outburst flood, threatening the local residents and buildings downstream of the dam and even causing significant damage [5][6][7][8][9]. Historically, many outburst floods have caused massive amounts of casualties and property losses, and even the extermination of civilizations [10]. For example, in 1786, the discharge of the Mogangling landslide dam outburst flood caused the deaths of approximately 100,000 people [11]. In 1967, the outburst flood of the Tanggudong landslide dam spread over 1,000 kilometers [12]. In 1933, approximately 2500 people were killed and disappeared during the outburst flood of the Diexi landslide dam [13]. However, emergency rescues are weakened by the lack of basic data. The damage of land and water transportation, the unpredictable nature of the surrounding environment, and the extremely short construction time In this study, the channel from the Baige landslide dam to the downstream Suwalong Hydropower Station was set as the research area. The entire process of the outburst flood was simulated. In addition, according to the actual design, the Yebatan arch dam is used to intercept the floods in two forms, namely, the complete interception and comprehensive flood control of blocking and draining. Therefore, the entire flood process with engineering interception combined with the  In the lower reaches of the Baige landslide-dammed lake, the construction of hydraulic buildings is planned, namely, the Gangtuo, Yanbi, Boluo, Yebatan, Lawa, Batang, and Suwalong Hydropower Stations, among which the Gangtuo, Yanbi, Boluo, and Lawa Stations are proposed, while the remainder are currently under construction (Figure 1b). The Baige landslide dam is located between the Boluo Hydropower Station and the Yebatan Hydropower Station. The dam is approximately 54.0 km upstream of the Yebatan Hydropower Station in Gaiyu Township, Baiyu County, Sichuan Province. The cascade power station downstream of the Baige landslide dam has not been completely constructed and thus did not play a role in this flood event. Assuming that one downstream hydraulic building has been constructed, can the dam reservoir accommodate an outburst flood or will an overtopping or even dam break occur, causing more damage to the downstream areas?
In this study, the channel from the Baige landslide dam to the downstream Suwalong Hydropower Station was set as the research area. The entire process of the outburst flood was simulated. In addition, according to the actual design, the Yebatan arch dam is used to intercept the floods in two forms, namely, the complete interception and comprehensive flood control of blocking and draining. Therefore, the entire flood process with engineering interception combined with the 3D inundation area was obtained.

Unsteady Flow Model Description
The unsteady flow modeling component of the Army Corps of Engineer's Hydrologic Engineering Center river analysis system (HEC-RAS; U.S. Army Corps of Engineers (USACE), developed by Barkau 1996) was used for dynamic flood routing in this study [20][21][22][23]. The basic HEC-RAS computational procedure for unsteady flow is based on a one-dimensional Saint Venant equation using an implicit, finite difference method [24,25]. The unsteady flow equation, which was adapted from Dr. Robert L. Barkau's UNET package of the continuity equation [26], is shown as follows: where A T is the total flow area at the midpoint of the control volume and Q is the flow at the midpoint of the control volume. The total flow area is the sum of the active area and off-channel storage area, and q l refers to the lateral inflow per unit length. The momentum equation used in the calculation is as follows: where Q is the discharge; V represents section velocity; ∂z ∂x is the water surface slope; S f is the friction slope; and A is the cross-sectional area.

Model Parameterization and Simulation Processes
In this study, three different datasets in the Jinsha River were used: (1) digital elevation model (DEM, download from Geospatial Data Cloud, 30 m resolution); (2) land cover data (30 m resolution); (3) flow curve of each site in the upper and middle reaches of the Jinsha River (provided by China Renewable Energy Engineering Institute). The methodology used in this research, which is presented in Figure 2, consisted of three main steps.
In step one, a digital elevation model was used to calculate the upper river network of the Jinsha River and generate a stream centerline. Taking the stream centerline as the river center, the riverbank and flow path were computed at distances of 50 m and 100 m, respectively. Subsequently, hundreds of cross-sections and five characteristic sections (cross-section at the Baige landslide dam, Yebatan arch dam, Lawa Hydropower Station, Batang Hydropower Station, and Suwalong Hydropower Station) were drawn to obtain the river/reach names, stations, bank stations, and downstream reach lengths. In addition, the natural channel roughness (Manning's n value) was analyzed statistically with the use of land cover data in combination with the natural channel roughness experience table. Then, the section details of the key section were obtained though the triangular irregular network (TIN), cross-section locations, and Manning's n values (n). storage area, and refers to the lateral inflow per unit length. The momentum equation used in the calculation is as follows: where Q is the discharge; V represents section velocity; is the water surface slope; Sf is the friction slope; and A is the cross-sectional area.

Model Parameterization and Simulation Processes
In this study, three different datasets in the Jinsha River were used: (1) digital elevation model (DEM, download from Geospatial Data Cloud, 30 m resolution); (2) land cover data (30 m resolution); (3) flow curve of each site in the upper and middle reaches of the Jinsha River (provided by China Renewable Energy Engineering Institute). The methodology used in this research, which is presented in Figure 2, consisted of three main steps. In step one, a digital elevation model was used to calculate the upper river network of the Jinsha River and generate a stream centerline. Taking the stream centerline as the river center, the riverbank and flow path were computed at distances of 50 m and 100 m, respectively. Subsequently, hundreds of cross-sections and five characteristic sections (cross-section at the Baige landslide dam, Yebatan arch dam, Lawa Hydropower Station, Batang Hydropower Station, and Suwalong Hydropower Station) were drawn to obtain the river/reach names, stations, bank stations, and downstream reach lengths. In addition, the natural channel roughness (Manning's n value) was analyzed statistically with the use of land cover data in combination with the natural channel roughness experience table. Then, the section details of the key section were obtained though the triangular irregular network (TIN), cross-section locations, and Manning's n values (n). In the second step, an unsteady flow of a one-dimensional hydraulic calculation was used to simulate the water surface of the Jinsha River. The Baige landslide dam was set as the water inlet, and the inlet flow data were obtained from the flood curve ( Figure 3, flood curve in red). The interpolation algorithm uncertainty and the DEM accuracy can be considered when the water level is interpolated on a DEM from the cross-sections [27]. Aronica et al. and Romanowicz and Beven applied fuzzy-based measures in the evaluation of a flood inundation model to allow for measurements with high uncertainties [28,29].
where F illustrates the degree of fuzzy fit. Sobs/Scomp are the set of observed and computed flooded cell/pixels, respectively. µ obs/com is the observed and computed membership value of the cells. ∆µ is the absolute difference between the observed and computed membership values of each cell. After model calibration, the simulation process is divided into two main categories (natural discharge and outburst flood with high dam interception). In the high dam interception simulation, the Yebatan arch dam was introduced downstream to intercept the flood. The dam gate was set as shown in Figure 4 with 5 crest outlets (12 m high × 11 m wide) and 4 deep holes (6 m high × 5 m wide). We simulated the flood process under two hydraulic building intercept conditions, as shown in Table 1, and the conditions divided into complete interception and comprehensive flood control of blocking and draining. In the 1st numerical simulation, the reservoir water level was set to 2700 m, and all gates were closed to simulate a timely interception. Historically, the collapse time of landslide dams are uncertain, and therefore, the downstream hydropower station may fail to drain the reservoir water in time [30]. The outburst flood may cause waves that overtop the dam and even lead to dam failure, Water 2020, 12, 605 5 of 17 which causes more damage. For this situation, we simulated the flood process in the most dangerous situation (Table 1, 2nd). The reservoir water level was set at 2855 m (dead water level), and all of the gates were opened. Subsequently, the entire flood process was simulated. In the final step, the data calculated in HEC-RAS were imported into ArcGIS for 3D flood inundation area calculations.
simulate the water surface of the Jinsha River. The Baige landslide dam was set as the water inlet, and the inlet flow data were obtained from the flood curve ( Figure 3, flood curve in red). The interpolation algorithm uncertainty and the DEM accuracy can be considered when the water level is interpolated on a DEM from the cross-sections [27]. Aronica et al. and Romanowicz and Beven applied fuzzy-based measures in the evaluation of a flood inundation model to allow for measurements with high uncertainties [28,29].
where F illustrates the degree of fuzzy fit. Sobs/Scomp are the set of observed and computed flooded cell/pixels, respectively. μobs/com is the observed and computed membership value of the cells. △μ is the absolute difference between the observed and computed membership values of each cell. After model calibration, the simulation process is divided into two main categories (natural discharge and outburst flood with high dam interception). In the high dam interception simulation, the Yebatan arch dam was introduced downstream to intercept the flood. The dam gate was set as shown in Figure 4 with 5 crest outlets (12 m high × 11 m wide) and 4 deep holes (6 m high × 5 m wide). We simulated the flood process under two hydraulic building intercept conditions, as shown in Table 1, and the conditions divided into complete interception and comprehensive flood control of blocking and draining. In the 1st numerical simulation, the reservoir water level was set to 2700 m, and all gates were closed to simulate a timely interception. Historically, the collapse time of landslide dams are uncertain, and therefore, the downstream hydropower station may fail to drain the reservoir water in time [30]. The outburst flood may cause waves that overtop the dam and even lead to dam failure, which causes more damage. For this situation, we simulated the flood process in the most dangerous situation (Table 1, 2nd). The reservoir water level was set at 2855 m (dead water level), and all of the gates were opened. Subsequently, the entire flood process was simulated. In the final step, the data calculated in HEC-RAS were imported into ArcGIS for 3D flood inundation area calculations.

Simulation Model Calibration
In this study, hydrological monitoring systems were set at four hydropower stations downstream of the Baige landslide dam, and the flow process was recorded ( Figure 3). The observed flow process at the Baige Landslide dam was set as the inlet flow data. Flow curves in the four downstream hydropower stations were calculated using the continuity equation and momentum equation. Preliminary studies considered the roughness parameter and geometry to be the most important indexes for the flood routing simulation [31][32][33]. HEC-RAS models of the Jinsha River were initially calibrated by minimizing the difference between the observed and modeled time-flow relationships by adjusting the value of n. Additional adjustments were made to n to best match the

Simulation Model Calibration
In this study, hydrological monitoring systems were set at four hydropower stations downstream of the Baige landslide dam, and the flow process was recorded ( Figure 3). The observed flow process at Water 2020, 12, 605 6 of 17 the Baige Landslide dam was set as the inlet flow data. Flow curves in the four downstream hydropower stations were calculated using the continuity equation and momentum equation. Preliminary studies considered the roughness parameter and geometry to be the most important indexes for the flood routing simulation [31][32][33]. HEC-RAS models of the Jinsha River were initially calibrated by minimizing the difference between the observed and modeled time-flow relationships by adjusting the value of n. Additional adjustments were made to n to best match the timing of the routed hydrograph peaks to those recorded at the downstream stations in the study reaches. The final calibrated n values of different land types were 0.04 for crop land, 0.02 for forest, 0.03 for grassland, 0.06 for shrub land, 0.035 for wetland, 0.023 for water, 0.02 for tundra, 0.035 for impervious surface, 0.035 for bare land, and 0.024 for snow/ice. The observed and simulated flow curves of the four downstream hydropower stations are shown in Figure 5. The simulation results agree well with the actual results, and the closer the location is to the position of the water inlet, the smaller the error will be.  The initial study considered that woody debris, meanders, and vegetation within the channel could reduce the flow velocity, resulting in the attenuation of flood flows [25]. Hence, the flood curve at the Batang and Suwalong Hydropower Stations in the simulation appeared ahead of the real flood curve (shown in Figure 5). The water surface curves of the flood process are shown in Figure 6. Notably, when the flood peak arrived at the Lawa hydropower station, the flood at the Baige landslide dam was completely discharged. While the flood peak arrived at the Suwalong Hydropower Station, the flood at the Yebatan arch dam was completely discharged. After 16 hours of flooding, the flood peak reached the Suwalong Hydropower Station with a channel distance of 224 km, which also resulted in a large inundation area. The three-dimensional display of the natural flood discharge when the flood reached the downstream area is shown in Figure 7. As shown in the figure, the downstream inundation area was more significant. In addition, the total inundation area and that in the downstream of the Yebatan arch dam are presented in Figure 7. The latter was calculated for comparison with the inundation area after the engineering interception. The total inundation area increased from 2.07 × 10 7 m 2 when the flood peak reached the Baige landslide dam to 2.64 × 10 7 m 2 when the flood peak reached the Batang Hydropower Station. When the flood peak 7 2   [25]. Hence, the flood curve at the Batang and Suwalong Hydropower Stations in the simulation appeared ahead of the real flood curve (shown in Figure 5). The water surface curves of the flood process are shown in Figure 6. Notably, when the flood peak arrived at the Lawa hydropower station, the flood at the Baige landslide dam was completely discharged. While the flood peak arrived at the Suwalong Hydropower Station, the flood at the Yebatan arch dam was completely discharged. After 16 hours of flooding, the flood peak reached the Suwalong Hydropower Station with a channel distance of 224 km, which also resulted in a large inundation area. The three-dimensional display of the natural flood discharge when the flood reached the downstream area is shown in Figure 7. As shown in the figure, the downstream inundation area was more significant. In addition, the total inundation area and that in the downstream of the Yebatan arch dam are presented in Figure 7. The latter was calculated for comparison with the inundation area after the engineering interception. The total inundation area increased from 2.07 × 10 7 m 2 when the flood peak reached the Baige landslide dam to 2.64 × 10 7 m 2 when the flood peak reached the Batang Hydropower Station. When the flood peak arrived at the Suwalong Hydropower Station, the total inundation area decreased to 2.58 × 10 7 m 2 , which may have resulted from the reduction in the upstream inundation area.     The numerical simulation results show that the Yebatan storage capacity can accommodate an outburst flood caused by the collapse of the Baige landslide dam. However, the reservoir capacity would be challenged by a continuous upstream water supply, and it is therefore unreasonable to use only interception. Moreover, the collapse time of the Baige landslide dam is uncertain, and the Yebatan Hydropower Station may not have an adequate amount of time to empty the reservoir water. Therefore, comprehensive flood control of blocking and draining may be an optimal choice. We simulated the flood process under the most dangerous conditions, that is, when the reservoir elevation is at the dead water level and the upstream dam breaks out. At this time, all gates of the Yebatan arch dam were opened (Table 1, 2nd). The settings for each gate are shown in Table 2. The gate opening and closing rates for all gates were 1 m/min. The maximum gate opening for the crest outlets and deep holes were 12 m and 6 m, respectively. In addition, the minimum gate opening and initial gate opening for these gates were all 0.5 m. The numerical simulation results show that the Yebatan storage capacity can accommodate an outburst flood caused by the collapse of the Baige landslide dam. However, the reservoir capacity would be challenged by a continuous upstream water supply, and it is therefore unreasonable to use only interception. Moreover, the collapse time of the Baige landslide dam is uncertain, and the Yebatan Hydropower Station may not have an adequate amount of time to empty the reservoir water. Therefore, comprehensive flood control of blocking and draining may be an optimal choice. We simulated the flood process under the most dangerous conditions, that is, when the reservoir elevation is at the dead water level and the upstream dam breaks out. At this time, all gates of the Yebatan arch dam were opened (Table 1, 2nd). The settings for each gate are shown in Table 2. The gate opening and closing rates for all gates were 1 m/min. The maximum gate opening for the crest outlets and deep holes were 12 m and 6 m, respectively. In addition, the minimum gate opening and initial gate opening for these gates were all 0.5 m.   Figure 9 shows that overtopping did not occur at the Yebatan arch dam. Furthermore, the flood curves are shown in Figure 10. All of the flood peaks of the hydropower station downstream of the Baige landslide dam were reduced sharply. The flood peaks at these four cascade hydropower stations were 8144 m 3 /s, 8818 m 3 /s, 8538 m 3 /s, and 6901 m 3 /s. The total inundation area and inundation area in the lower part of the Yebatan arch dam are shown in Figure 11. These two inundation areas both showed an increasing trend, and the inundation area in the lower part of the Yebatan arch dam was much smaller than the total inundation area. In addition, Figure 11 also shows the inundation area of the basin as the flood reached the downstream area. The figure shows that after the flood is mainly concentrated behind the Yebatan arch dam, the water depth at the downstream Suwalong Hydropower Station is relatively shallow.    Figure 9 shows that overtopping did not occur at the Yebatan arch dam. Furthermore, the flood curves are shown in Figure 10. All of the flood peaks of the hydropower station downstream of the Baige landslide dam were reduced sharply. The flood peaks at these four cascade hydropower stations were 8144 m 3 /s, 8818 m 3 /s, 8538 m 3 /s, and 6901 m 3 /s. The total inundation area and inundation area in the lower part of the Yebatan arch dam are shown in Figure 11. These two inundation areas both showed an increasing trend, and the inundation area in the lower part of the Yebatan arch dam was much smaller than the total inundation area. In addition, Figure 11 also shows the inundation area of the basin as the flood reached the downstream area. The figure shows that after the flood is mainly concentrated behind the Yebatan arch dam, the water depth at the downstream Suwalong Hydropower Station is relatively shallow. Water 2020, 12, x FOR PEER REVIEW 11 of 18

Maximum Water Depth Lag Effect
In this numerical simulation, the maximum water depth exhibited a time-lag effect compared to the maximum outburst flood. Taking the natural discharge as an example, the maximum water depth lagged behind the maximum outburst flood for different periods of time (shown in Figure 12). Specifically, the maximum water level was approximately 4 hours, 6 hours, 6.5 hours, and 6 hours at the Baige landslide dam, Yebatan arch dam, Lawa Hydropower Station, Batang Hydropower Station, and Suwalong Hydropower Station. The reason for this phenomenon is as follows.

Flood Peak Discharge
The Yebatan Hydropower Station with its gate completely closed can accommodate outburst flooding and thus eliminate the flood risk when the initial reservoir elevation is reduced to 2700 m. When conducting comprehensive flood control of blocking and draining, the flood peak was noticeably reduced, and the flood peak arrival time was significantly delayed compared with the natural discharge. As shown in Figure 13, the flood peak discharge decreased by 20,156 m 3 /s, 11,874 m 3 /s, 11,876 m 3 /s, and 10,465 m 3 /s at the Yebatan arch dam, Lawa hydropower station, Batang hydropower station, and Suwalong hydropower station, respectively. Compared with the flood curve without a dam, the flood peaks of every hydrological monitoring point with a dam decreased. Moreover, this indicates that the closer the location is to the Baige landslide dam, the more obvious the reduction in the flood peak will be. Moreover, the flood peak arrival time did not show an obvious delay, and those of the Lawa hydropower station, Batang hydropower station, and Suwalong hydropower station were 3.75 h, 3.75 h, and 5.75 h, respectively. The delayed time showed a gradual increase, and this phenomenon indicates that the closer the location is to the Baige landslide dam, the more obvious the increase in the flood peak arrival time will be.
Hydraulic buildings, such as hydropower stations, clearly reduced the flood peak and delayed the peak flood arrival time, directly reducing the inundation area of downstream farmland and increasing the evacuation time for the downstream residents, indirectly protecting the property and safety of local residents. The formula for the section-specific energy is as follows: where E S represents the section-specific energy, h represents the water depth, and V represents the sectional velocity.
When the section-specific energy, section form, and size are fixed, Q = F(H) fits into the above formula. After plotting the relationship between Q and h, the figure shows that when the first derivative is taken by Equation (6) of h, Q = F(H) obtains the maximum value. The first derivative is as follows: When dQ dh = 0, the maximum value of Q = F(h) can be obtained as follows: given that and so 2B( And substituting Formula (5) into Formula (10), When the section-specific energy, section form, and size are constant, the maximum outburst flood corresponds to the critical water depth (obtained from Equation (11)). The maximum water depth occurs after the critical water depth, so the maximum water depth exhibits a time-delay effect compared to the maximum flow rate.

Flood Peak Discharge
The Yebatan Hydropower Station with its gate completely closed can accommodate outburst flooding and thus eliminate the flood risk when the initial reservoir elevation is reduced to 2700 m. When conducting comprehensive flood control of blocking and draining, the flood peak was noticeably reduced, and the flood peak arrival time was significantly delayed compared with the natural discharge. As shown in Figure 13, the flood peak discharge decreased by 20,156 m 3 /s, 11,874 m 3 /s, 11,876 m 3 /s, and 10,465 m 3 /s at the Yebatan arch dam, Lawa hydropower station, Batang hydropower station, and Suwalong hydropower station, respectively. Compared with the flood curve without a dam, the flood peaks of every hydrological monitoring point with a dam decreased. Moreover, this indicates that the closer the location is to the Baige landslide dam, the more obvious the reduction in the flood peak will be. Moreover, the flood peak arrival time did not show an obvious delay, and those of the Lawa hydropower station, Batang hydropower station, and Suwalong hydropower station were 3.75 h, 3.75 h, and 5.75 h, respectively. The delayed time showed a gradual increase, and this phenomenon indicates that the closer the location is to the Baige landslide dam, the more obvious the increase in the flood peak arrival time will be.

Water Depth
There are also differences in water depths between natural discharge and comprehensive flood control of blocking and draining. Figure 14 presents the maximum water depth of all sections with or without engineering interception. The figure shows that the water depth behind the dam was as much as approximately 200 m, and the water depth increased by nearly 150 m compared with the water levels without high dam interception. In addition, near the downstream area of the arch dam, the water depth of the natural discharge was also deeper than that of high dam interception. In the Hydraulic buildings, such as hydropower stations, clearly reduced the flood peak and delayed the peak flood arrival time, directly reducing the inundation area of downstream farmland and increasing the evacuation time for the downstream residents, indirectly protecting the property and safety of local residents.

Water Depth
There are also differences in water depths between natural discharge and comprehensive flood control of blocking and draining. Figure 14 presents the maximum water depth of all sections with or without engineering interception. The figure shows that the water depth behind the dam was as much as approximately 200 m, and the water depth increased by nearly 150 m compared with the water levels without high dam interception. In addition, near the downstream area of the arch dam, the water depth of the natural discharge was also deeper than that of high dam interception. In the lower reaches of the Yebatan arch dam, the water depth was approximately 20 to 30 m and 10 to 20 m for natural discharge and with high dam interception, respectively. The water depth with high dam interception was reduced by approximately 10 m compared to that without high dam interception. The water depth is directly related to the inundation area and is a very important index that is used to describe the flood process. A ten-meter reduction in the downstream water depth means that the downstream flood risks were greatly reduced.

Water Depth
There are also differences in water depths between natural discharge and comprehensive flood control of blocking and draining. Figure 14 presents the maximum water depth of all sections with or without engineering interception. The figure shows that the water depth behind the dam was as much as approximately 200 m, and the water depth increased by nearly 150 m compared with the water levels without high dam interception. In addition, near the downstream area of the arch dam, the water depth of the natural discharge was also deeper than that of high dam interception. In the lower reaches of the Yebatan arch dam, the water depth was approximately 20 to 30 m and 10 to 20 m for natural discharge and with high dam interception, respectively. The water depth with high dam interception was reduced by approximately 10 m compared to that without high dam interception. The water depth is directly related to the inundation area and is a very important index that is used to describe the flood process. A ten-meter reduction in the downstream water depth means that the downstream flood risks were greatly reduced.

Inundation Area
The entire flooding process is a disaster-causing process, which includes the flooding of farmland and the destruction of houses. The natural discharge of the Baige landslide dam has caused significant losses downstream. When considering the comprehensive flood control of blocking and draining, the flood process also undergoes tremendous changes in the most dangerous situations. Figure 15 demonstrates the inundation areas of both the natural discharge and high dam interception. This figure shows the inundation area downstream of the Yebatan arch dam when the flood peak reached the Baige landslide dam, Yebatan arch dam, Lawa hydropower station, Batang hydropower station, and Suwalong hydropower station. For the natural discharge, the flood peaks evolved downstream, and the inundation area increased at a faster rate. When the flood peak reached the Lawa Hydropower Station, the inundation area close to the Yebatan arch dam gradually decreased due to discharge, and although the inundation area in the downstream area increased rapidly, the total flooded area showed a tendency to slowly increase. When there was high dam interception, the inundation area showed a slow growth trend. The inundation area after engineering interception was greatly reduced, and the area of the downstream inundation area was more obvious. When the flood peak arrived at the Baige landslide dam and Yebatan hydropower station, the inundation area decreased by approximately 20%. When the flood evolved to the Lawa hydropower station, the Batang hydropower station, and the Suwalong hydropower station, the inundation area reduced to half of that for the natural discharge. The reduction in the inundation area from the construction of dams can effectively reduce the risk of downstream disasters.
reached the Lawa Hydropower Station, the inundation area close to the Yebatan arch dam gradually decreased due to discharge, and although the inundation area in the downstream area increased rapidly, the total flooded area showed a tendency to slowly increase. When there was high dam interception, the inundation area showed a slow growth trend. The inundation area after engineering interception was greatly reduced, and the area of the downstream inundation area was more obvious. When the flood peak arrived at the Baige landslide dam and Yebatan hydropower station, the inundation area decreased by approximately 20%. When the flood evolved to the Lawa hydropower station, the Batang hydropower station, and the Suwalong hydropower station, the inundation area reduced to half of that for the natural discharge. The reduction in the inundation area from the construction of dams can effectively reduce the risk of downstream disasters.

Conclusions
In this study, an unsteady flow from a one-dimensional hydraulic calculation was used to simulate outburst flood routing in both natural discharge and high dam interception. The dynamic responses of the outburst flow, water surface curve, water depth, and inundation area for the natural discharge are obtained and comprehensively analyzed. In addition, the Yebatan arch dam was set up according to the design, and the flood process was simulated by means of complete interception and comprehensive flood control of blocking and draining, verifying the safety of the project and analyzing the possibility of hydraulic building disaster reduction. The results are summarized below.

Conclusions
In this study, an unsteady flow from a one-dimensional hydraulic calculation was used to simulate outburst flood routing in both natural discharge and high dam interception. The dynamic responses of the outburst flow, water surface curve, water depth, and inundation area for the natural discharge are obtained and comprehensively analyzed. In addition, the Yebatan arch dam was set up according to the design, and the flood process was simulated by means of complete interception and comprehensive flood control of blocking and draining, verifying the safety of the project and analyzing the possibility of hydraulic building disaster reduction. The results are summarized below.
(1) During the flood process, the maximum water depth exhibited a time-lag effect compared to the maximum outburst flood. The time lag varies according to roughness.
(2) The reservoir of the Yebatan arch dam can accommodate the outburst flood of the Baige landslide dam, and the reservoir has a remaining capacity.
(3) In the most dangerous situation, outburst floods can be safely discharged without generating an overtopping disaster when all gates are fully opened to discharge the flood.
(4) When conducting comprehensive flood control of blocking and draining, the flood peak was noticeably reduced and the flood peak arrival time was significantly delayed compared with the natural discharge. Specifically, the flood peak decreased more obviously when it was closer to the upstream area, and the flood peak arrival time was more delayed when the flood spread further downstream.
(5) When conducting comprehensive flood control of blocking and draining, the water depth in the downstream area of the Yebatan arch dam was reduced by approximately 10 m and the inundation area was reduced by approximately half of that in the natural discharge.
(6) Engineering interception has extremely important significance for disaster reduction. Engineering interception can reduce the inundation area of downstream land, thus reducing the loss of crops and ecological damage. In addition, engineering interception can extend the evacuation time for local residents, which greatly reduces casualties.
Pure water was used for the simulation in this study, which is different from the actual situation of water and sand coupling. In addition, the inaccuracy of the terrain data in large areas can affect the simulation results. Therefore, improving the accuracy of the terrain data and simulating the water-sand coupled flood process using measured sediment data is worth further study.