Floods are among the most prevalent natural disasters, posing significant threats to human activities. Reservoirs can enhance flood control and water conservation by using flood forecast information to prerelease water or adjust storage. However, making timely pre-release decisions that balance reservoir safety and downstream conditions remains challenging. This study aims to develop a reservoir operation model that helps reduce peak releases during the flood season, generate reference tables and graphs for determining target reservoir elevation after pre-release, and propose practical applications for real-time decision-making. We evaluated five flood operation methods (FOMs) using this model and identified FOM V as the most effective. We conducted three case studies on extreme flood events in the Seomjingang reservoir and validated the model using data from the Hapcheon reservoir. The model produces reference graphs and tables to guide operators in determining the target reservoir elevation based on forecasted inflow, updated with each new forecast. The novelty of this study lies in offering a simple, user-friendly tool that enables prompt and reliable reservoir operation during flood events. Our approach supports real-time, proactive reservoir management, reducing downstream flood damage and ensuring sufficient water supply for the dry season.

  • Developed reservoir operation models that guide operators in reducing peak releases.

  • Generated reference tables and graphs to decide the target reservoir elevation after pre-release.

  • Supported decision-making that prevents dam failure and reduces downstream damage.

Rising global temperatures intensify the hydrological cycle, driving more frequent and severe rainfall events, accelerating snowmelt, and increasing sea levels, all of which amplify the risk and impact of flooding (Lee et al. 2023a, 2023b). Reservoirs play a crucial role in mitigating flood risks and are a cornerstone of effective flood management (Yi & Yi 2024). However, with growing environmental awareness, there is a shift from constructing new reservoirs to optimizing the use of existing ones for flood control. One of the most effective approaches to enhancing flood management is investigating the potential of pre-release strategies (Chen et al. 2013). Reservoirs can strategically pre-store or prerelease flows for flood control or water conservation (Cheng & Chau 2001; Karaboga et al. 2008). Pre-storage is retaining more water in the reservoir to reduce the risk of water shortages in case the anticipated flood does not occur (Li et al. 2010). Pre-release mitigates flood severity by providing reservoir space to hold anticipated inflows during the severe storm events (Jain et al. 1992; Mediero et al. 2007).

The pre-release approach aims to make flood control storage available before storm events, thereby enhancing flood management and reducing flood damage (Ghobadi & Kaboli 2020; Rezay Nazarzadeh et al. 2020). This strategy helps avoid or reduce the use of emergency spillway gates, which can lead to unplanned, sudden increases in releases and potentially cause severe downstream damage (Krzysztofowicz & Duckstein 1979). Pre-releasing water is a common practice in various countries to manage flood risks effectively (Hidayah Ishak & Mustafa Hashim 2018; Endo et al. 2020; Fujita & Kanae 2023). Determining the pre-release strategy requires a careful balance between reducing flood risks and ensuring water conservation. Operational rules, for example, often aim to maintain sufficient flood control storage; however, this approach may necessitate the unnecessary opening of reservoir spillway gates, potentially leading to water shortages post-flood season (Liu et al. 2006). While releasing water in advance can reduce flood impacts, it also involves uncertainties from forecasted meteorological and hydrological data (Lu et al. 2022). Enhancing the accuracy of forecasted meteorological and hydrological data to improve reservoir flood control operations is a popular topic (Beven 1993; Wei et al. 2018).

The pre-release strategy has consistently demonstrated its effectiveness in managing reservoir storage, reducing flood risks, and preventing reservoir failure during storm events (Alfieri et al. 2017). Studies comparing scenarios with and without pre-release highlight its ability to manage storage efficiently during extreme inflows (Hossain et al. 2020). Decision support tools that utilize real-time flood forecasts further enhance pre-release planning, allowing operators to act proactively before events like typhoons. This approach significantly improves flood control outcomes without compromising water supply security (Chou & Wu 2013). Pre-release strategies also contribute to evenly distributed water releases, which reduce peak flows at downstream protection points, strengthen downstream flood resilience, and maintain reservoir safety (Wei et al. 2022). Recent advancements include the development of pre-release indices and refined scheduling models, which effectively prevent floods while maintaining water supply reliability. These models provide practical tools for reservoir operators to enhance flood management and safety (Huang et al. 2024). Furthermore, hierarchical pre-release flood operation rules, incorporating flood forecasts and uncertainty information, have been proposed to optimize real-time flood control. Multi-objective optimization models that account for multiple goals – such as flood control, power generation, and navigation – are being developed and optimized using advanced algorithms, offering a comprehensive approach to cascade reservoir operations (Liu et al. 2024).

Various methodologies have been developed to assess and enhance pre-release strategies in reservoir management. Many studies emphasize the role of inflow, precipitation, and surface runoff in revising reservoir intake estimations, as seen in the formulation of release equations based on probable maximum precipitation (Hossain et al. 2020). Pre-release strategies often aim to minimize downstream flood risks while achieving targeted water levels post-flood events (Nguyen et al. 2020). Optimization techniques have also been extensively explored, employing methods such as multi-objective optimization models (Dobson et al. 2019), fuzzy optimization models (Meng & Wu 2013), optimization-simulation models (Kim et al. 2021), stochastic reservoir operation optimization models (Celeste & Billib 2009), and artificial intelligence-based models (Chaves & Chang 2008). While these models perform well under specific conditions and constraints, their practical application poses challenges. For instance, optimization models can sometimes produce infeasible or impractical solutions, complicating their use in real-world operations (Chen et al. 2024). Effective decision-making must also consider reservoir flood control capacity to avoid exceeding downstream channel limits (Jiang et al. 2022). Moreover, prompt decision-making during flood events remains a critical operational challenge (Rezay Nazarzadeh et al. 2020).

Although numerous pre-release operation plans have been developed using various criteria and successfully applied to reservoir flood control, there is limited research on reservoir operation models that determine release volumes based on inflow while also considering downstream (control point) flood conditions in real time. Few studies have explored the timing and quantity of target pre-release in detail. To address these gaps, this study proposes an innovative approach that incorporates the target reservoir elevation by determining how much the water level should be pre-adjusted (controlled) to minimize downstream damage, taking inflow into account. This approach generates a reference graph that assists in determining the target reservoir elevation after the pre-release. A key advantage of this approach is its adaptability; as the forecasted flood event changes in real-time, the reference graph is recalculated, enabling operators to adjust release volumes dynamically to achieve the target reservoir elevation.

The main objectives are (A) developing a reservoir operation model that guides the operators to reduce peak release in flood season, (B) generating reference tables and graphs to determine the target reservoir elevation after pre-release, and (C) proposing practical applications for prompt decision-making in real-time reservoir operation. We selected the Seomjingang reservoir for this study because its downstream areas are prone to flooding. The Seomjingang reservoir has a historical record of not fully utilizing its flood control storage, as its previous model did not account for target pre-release during the flood season; in contrast, this study introduces a model that incorporates pre-release strategies. By integrating forecasted inflow and downstream control point conditions, this study provides a more efficient approach to reservoir operation, including determining the maximum release at a specific water level. We conduct three case studies on severe flood events in the Seomjingang reservoir and validate the model using data from the Hapcheon reservoir.

Most reservoirs in South Korea lack established pre-release strategies to prepare for upcoming floods. The novelty of this study is developing strategies that determine the timing and quantity of target pre-release, accounting for both reservoir inflow and downstream conditions. It also provides user-friendly reference graphs and tables to support operators in making prompt and reliable reservoir operation decisions during flood events. These tools dynamically update with new forecasted inflow data at each time step, enabling real-time decision-making. The proposed pre-release strategy can potentially reduce the risk of downstream flooding and reservoir failure. The potential impact of this study lies in its contribution to improved flood management practices and reservoir operation strategies. With the newly developed pre-release strategy, the flood control storage can be fully utilized for more effective flood management.

Study area

The five major river basins in South Korea are the Han River, Nakdong River, Geum River, Yeongsan River, and Seomjin River. In South Korea, 70% of the annual precipitation falls during the flood season (June–September), making flood control particularly challenging. With two-thirds of the country covered by mountains, heavy storms quickly flow downstream in a short period. To address these challenges, South Korea built 20 multipurpose reservoirs and three flood control reservoirs. These reservoirs store water during storms and release it after the storm passes, ensuring sufficient storage for the next floods.

The Seomjin River basin has two multipurpose reservoirs (Juam and Seomjingang reservoirs) and one hydropower reservoir (Boseonggang reservoir). Juam reservoir is downstream of the Boseonggang reservoir supplies industrial and municipal water to downstream areas and serves as a flood control reservoir (60 MCM) during the flood season. Boseonggang reservoir is at the uppermost reach of the Boseong River (the largest tributary of the Seomjin River). As a hydropower reservoir, it has limited flood control capacity (1 MCM). During the heavy rainfall, it releases water through the spillway into the Boseong River.

The Seomjingang reservoir, built in 1965, is South Korea's first multipurpose reservoir. It is located at the uppermost part of the Seomjin River (Figure 1). The basin area of this reservoir is 763.0 km2, which is 15.5% of the total watershed area (4,912.0 km2). It supplies agricultural, domestic, and industrial water. Despite having a flood control capability, it has limited flood control storage – only 30.3 MCM, or 6.5% of its total capacity of 466.0 MCM. This limited flood control storage is insufficient for flood management during the rainy season.
Figure 1

The study area is the Seomjingang reservoir located in the Seomjin River basin, South Korea. The river basin is in the upper part of the Seomjin River. The 2020 heavy storm caused significant flooding in the downstream areas, including Gokseong-eup and Geumji-myeon.

Figure 1

The study area is the Seomjingang reservoir located in the Seomjin River basin, South Korea. The river basin is in the upper part of the Seomjin River. The 2020 heavy storm caused significant flooding in the downstream areas, including Gokseong-eup and Geumji-myeon.

Close modal
We chose the Seomjingang reservoir as our study area because its downstream areas are prone to flooding, and there is a historical record of not fully utilizing its flood control storage. The 2020 flood exceeded the previous maximum elevation that caused downstream flooding. The government concluded that the cause of the downstream flooding and the failure of flood control in the reservoir was due to insufficient flood control storage and the changing climate. In 2021, the government launched a temporary plan to triple the reservoir's flood control capacity to 90.0 MCM by setting a restricted water level at 194.0 EL.m (Figure 2, Table 1).
Table 1

The maximum release capacity for the spillway gates opening at different reservoir elevations in the Seomjingang reservoir

Reservoir elevation (EL.m)Maximum release (CMS)Reservoir elevation (EL.m)Maximum release (CMS)
186.7 0.0 192.8 1,217.2 
186.8 2.0 192.9 1,261.2 
186.9 6.0 193.0 1,309.7 
187.0 10.8 193.1 1,370.8 
187.1 16.8 193.2 1,436.3 
187.2 23.6 193.3 1,503.4 
187.3 31.2 193.4 1,573.4 
187.4 39.2 193.5 1,645.0 
187.5 48.4 193.6 1,719.5 
187.6 58.0 193.7 1,797.1 
187.7 68.0 194.0 1,951.1 
188.0 102.4 194.5 2,363.0 
188.5 171.6 195.0 2,837.9 
189.0 252.4 195.5 3,382.0 
189.5 344.4 196.0 3,981.6 
190.0 446.8 196.5 4,603.6 
190.5 559.2 197.0 5,248.1 
191.0 681.6 197.5 5,902.7 
191.5 813.6 198.0 6,581.3 
192.0 964.4 198.5 7,289.0 
192.5 1,115.2 199.0 8,019.2 
192.6 1,147.2 200.0 9,551.9 
192.7 1,179.2 201.0 11,154.3 
Reservoir elevation (EL.m)Maximum release (CMS)Reservoir elevation (EL.m)Maximum release (CMS)
186.7 0.0 192.8 1,217.2 
186.8 2.0 192.9 1,261.2 
186.9 6.0 193.0 1,309.7 
187.0 10.8 193.1 1,370.8 
187.1 16.8 193.2 1,436.3 
187.2 23.6 193.3 1,503.4 
187.3 31.2 193.4 1,573.4 
187.4 39.2 193.5 1,645.0 
187.5 48.4 193.6 1,719.5 
187.6 58.0 193.7 1,797.1 
187.7 68.0 194.0 1,951.1 
188.0 102.4 194.5 2,363.0 
188.5 171.6 195.0 2,837.9 
189.0 252.4 195.5 3,382.0 
189.5 344.4 196.0 3,981.6 
190.0 446.8 196.5 4,603.6 
190.5 559.2 197.0 5,248.1 
191.0 681.6 197.5 5,902.7 
191.5 813.6 198.0 6,581.3 
192.0 964.4 198.5 7,289.0 
192.5 1,115.2 199.0 8,019.2 
192.6 1,147.2 200.0 9,551.9 
192.7 1,179.2 201.0 11,154.3 

Note. The spillway gates releases water when the reservoir elevation is between 186.7 and 201.0 m. The maximum release is 11,154.3 m3/s (CMS).

Figure 2

The Seomjingang reservoir features variable reservoir elevation configurations, accommodating distinct allocations for flood control storage, conservation storage, and inactive storage tailored to the needs of both flood and dry seasons.

Figure 2

The Seomjingang reservoir features variable reservoir elevation configurations, accommodating distinct allocations for flood control storage, conservation storage, and inactive storage tailored to the needs of both flood and dry seasons.

Close modal

Design flood in the reservoir and stream

In South Korea, the design flood for the reservoir is determined during the reservoir planning stage. The design flood ensures structural safety and prevents reservoir failure due to overtopping. The design flood is crucial for setting the flood water level and flood control storage capacities. The 200-year flood frequency is commonly used as the standard for the design flood. In some cases, we occasionally use smaller design floods than the 200-year flood frequency. The Seomjingang reservoir has a design flood of 2,953.0 CMS (200-year flood frequency), with a design release (of 1,810.0 CMS). The design release is the maximum release estimated through reservoir flood routing. The design flood for the stream is the maximum discharge that flows in the channel considering the upstream reservoir. All downstream sections of the Seomjin River use a 100-year frequency for design flood. The use of a 200-year flood frequency for the reservoir, compared to a 100-year flood frequency for downstream rivers, can cause conflicts in flood management. The flood stages for streams are classified into concern, caution, alert, and emergency stages (Table 2). The concern stage is when water reaches a level that overtops the intake facilities. The caution stage is the level at which a flood watch is issued. The alert stage is the level at which a flood warning is issued. The emergency stage is the river level that exceeds the designed flood level.

Table 2

The four flood stages are caution, alert, warning, and serious

CriteriaDescriptionActions
Caution This level is reached when the river stage is high enough to submerge major river-friendly facilities and vulnerable structures (such as bicycle paths and riverbanks) 
  • Prohibiting entry to river areas

  • Evacuating vehicles from nearby parking lots

  • Closing river walkways

  • Banning water-related activities

 
Alert Corresponds to 50% of the design flood (flood watch) 
  • Operating drainage pumps

  • Increasing patrols in vulnerable sections of levees

  • Reviewing potential evacuation areas for residents

 
Warning At 70% of the design flood (flood warning) 
  • Preparing for the potential breach or loss of levees and bridges

  • Inspecting vulnerable sections of levees

  • Preparing for emergency repairs

  • Controlling access to vulnerable bridges

 
Serious When the river stage reaches the design flood level. 
  • Preparing for levee breaches and overflows

  • Evacuating residents from low-lying areas

  • Implementing emergency repair measures

 
CriteriaDescriptionActions
Caution This level is reached when the river stage is high enough to submerge major river-friendly facilities and vulnerable structures (such as bicycle paths and riverbanks) 
  • Prohibiting entry to river areas

  • Evacuating vehicles from nearby parking lots

  • Closing river walkways

  • Banning water-related activities

 
Alert Corresponds to 50% of the design flood (flood watch) 
  • Operating drainage pumps

  • Increasing patrols in vulnerable sections of levees

  • Reviewing potential evacuation areas for residents

 
Warning At 70% of the design flood (flood warning) 
  • Preparing for the potential breach or loss of levees and bridges

  • Inspecting vulnerable sections of levees

  • Preparing for emergency repairs

  • Controlling access to vulnerable bridges

 
Serious When the river stage reaches the design flood level. 
  • Preparing for levee breaches and overflows

  • Evacuating residents from low-lying areas

  • Implementing emergency repair measures

 

Note. It outlines each stage and specifies the actions taken at each one.

In Figure 3, the heavy storm in 2020 caused significant flooding in the downstream areas of the Seomjin River near Gokseong-eup and Geumji-myeon. The design flood for the river section between these two areas is 5,590.0 CMS. This flood was caused by the most severe recent storm where the water level at the Seomjin reservoir exceeded the flood water level. At the Gokseong-eup river stage station, the river level overtopped the emergency stage, which caused widespread flooding in the area. Figure 4 displays the 2010 hydrograph, where the reservoir released between 700.0 and 800.0 CMS (38 and 44% of the design release). Despite these relatively small releases, the river level at the downstream observation station reached the alert stage. Both reservoir releases and tributary flows between the reservoir and flood-impacted areas resulted in damage. It is essential to consider both reservoir and downstream conditions when determining releases to minimize flood damage.
Figure 3

(a) The inflow, release, and reservoir elevation data for the Seomjingang Reservoir from August 2020. The reservoir release remained below the design release of 1,810.0 CMS, but the reservoir elevation exceeded the flood water level for approximately seven hours. (b)–(d) Streamflow and river level data from the Gokseong-eup observation station. The streamflow surpassed the design flow for about 12 h (c), while the river level exceeded the caution stage on 7th August and rose above the alert stage on 8th August (d).

Figure 3

(a) The inflow, release, and reservoir elevation data for the Seomjingang Reservoir from August 2020. The reservoir release remained below the design release of 1,810.0 CMS, but the reservoir elevation exceeded the flood water level for approximately seven hours. (b)–(d) Streamflow and river level data from the Gokseong-eup observation station. The streamflow surpassed the design flow for about 12 h (c), while the river level exceeded the caution stage on 7th August and rose above the alert stage on 8th August (d).

Close modal
Figure 4

(a) The inflow, release, and reservoir elevation data for the Seomjingang Reservoir from August 2010. Reservoir releases remained between 700.0 and 800.0 CMS, below the design release of 1,810.0 CMS, and the reservoir elevation stayed below the flood water level. (b)–(d) Streamflow and river stage data from the Gokseong-eup observation station. The streamflow was kept below the design flow (c), but the river stage exceeded the alert level (d).

Figure 4

(a) The inflow, release, and reservoir elevation data for the Seomjingang Reservoir from August 2010. Reservoir releases remained between 700.0 and 800.0 CMS, below the design release of 1,810.0 CMS, and the reservoir elevation stayed below the flood water level. (b)–(d) Streamflow and river stage data from the Gokseong-eup observation station. The streamflow was kept below the design flow (c), but the river stage exceeded the alert level (d).

Close modal

Flood operation method

The five flood operation methods (FOMs) are commonly used for operating multipurpose reservoirs in South Korea (Table 3) (Figure 5). We use the term FOM which emphasizes the flood operation, while the term reservoir operation method is commonly used as a reservoir operation technique for flood control (Yoo et al. 2020).
Table 3

Most reservoirs use FOM II and FOM V

FOMReservoirs
FOM II Boyeong, Bunhang, Chungju, Daecheong, Gimcheon, Gunwi, Hoengseong, Hapcheon, Imha, Juam, Milyang, Yongdam 
FOM III and pre-release Namgang 
FOM V Andong, Bohyunsan, Janheung, Seomjingang, Seongdeok, Soyanggang 
Overflow spillway Buan 
FOMReservoirs
FOM II Boyeong, Bunhang, Chungju, Daecheong, Gimcheon, Gunwi, Hoengseong, Hapcheon, Imha, Juam, Milyang, Yongdam 
FOM III and pre-release Namgang 
FOM V Andong, Bohyunsan, Janheung, Seomjingang, Seongdeok, Soyanggang 
Overflow spillway Buan 

Note. The Seomjingang reservoir uses FOM V (efficient utilization strategies for existing water resources, K-water, 2019).

Figure 5

Five FOMs, which (a) represents FOM I, (b) FOM II, (c) FOM III, (d) FOM IV, and (e) FOM V. Dashed lines represent reservoir elevation, dotted lines indicate release, solid lines represent inflow, and the grey shaded area represents the storage reserved for flood control storage.

Figure 5

Five FOMs, which (a) represents FOM I, (b) FOM II, (c) FOM III, (d) FOM IV, and (e) FOM V. Dashed lines represent reservoir elevation, dotted lines indicate release, solid lines represent inflow, and the grey shaded area represents the storage reserved for flood control storage.

Close modal
FOM I involves retaining all incoming water until the reservoir elevation reaches the flood water level, at which point it releases water at a rate equal to the inflow. This approach, while used in small reservoirs with simple, ungated spillways, poses a risk of reservoir failure from overtopping in larger reservoirs, as it delays action until the flood water level is reached. Such delays can lead to downstream flood damage due to excessive releases, failing to make full use of the reservoir flood control capacity. According to the following equation, if the storage is below the flood storage threshold, no water is released; otherwise, the release is the same as the inflow.
(1)
where represents the release at time t, is the storage of the reservoir at time t, denotes the storage of the flood water level, and represents the forecasted inflow to the reservoir at time t.
FOM II is based on a fixed-rate-fixed-amount approach. The release is calculated by multiplying the inflow by a predetermined ratio to release water at a constant rate. Once the inflow decreases, the current release is maintained until the reservoir level reaches the restricted water level. However, for the double-peak inflow event, the inflow may exceed the release before the reservoir elevation reduces to the restricted water level. In this case, the release is increased by applying the fixed rate again until the reservoir elevation is lowered to the restricted water level, maintaining the release from the point of the second peak inflow. The limitation of FOM II is involving the complex spillway gate operation and applying it to multiple peak inflows.
(2)
(3)
where r represents the ratio used in FOM II, and t denotes time.
Based on the forecasted inflow, FOM III calculates a constant release to utilize the full flood control capacity. We release all inflow until it becomes the same as the determined release. Once they are the same, we maintain a constant release. FOM III is considered the most effective flood control method, assuming reliable inflow forecasting is available. FOM III faces limitations when the input dataset is updated at short intervals, requiring frequent recalculations of the predetermined constant release. The following equation determines the release for FOM III.
(4)
where represents the time when the reservoir elevation exceeds the normal high water level (or the restricted water level in flood season), prompting the start of spillway release, while indicates the time when the reservoir elevation reaches the flood water level. denotes the storage of the normal high water level and denotes the storage of the restricted water level.

FOM IV makes releases based on predetermined amounts by the reservoir level alone, disregarding inflow volume. This method uses a predefined spillway rule curve (SRC), which is based on the design flood. The SRC considers the size of the reservoir, flood control capacity, and spillway gate release capabilities to determine release for varying reservoir elevations. However, this approach may not accurately reflect actual flood conditions if the inflow significantly differs from the design flood.

FOM V makes a constant release based on the predefined rules for each reservoir. When the storage of the reservoir is smaller than the storage of the flood water level and the inflow is less than the design release, then the release is the same as the inflow. However, if the inflow is larger than the design release, a constant release is maintained. When the reservoir storage exceeds the storage of the flood water level, it fully opens the spillway gates and releases all incoming flow.
(5)
where D represents the design release, and C represents the constant release.

Development of reservoir simulation model

We develop a reservoir simulation model that can run five FOMs. The model determines the target reservoir elevation after pre-release based on forecasted inflow. The target reservoir elevation is defined as the elevation after it has been lowered through pre-release, prior to starting flood operations. Figure 6 illustrates the workflow of this study. First, we collect input data, including the characteristics of a reservoir and information essential for operation. Second, we need additional information on the starting reservoir elevation and maximum reservoir elevation for the selected reservoir. Then, we choose which FOM to run the model and determine whether the resulting peak release is larger or smaller than the downstream target design flood. Reservoir operations are repeated by adjusting the target reservoir elevation until the desired peak release is obtained while considering the downstream flood conditions. We apply the developed reservoir simulation model to three case studies in the Seomjingang reservoir and validate it using data from the Hapcheon reservoir. Python was the main coding language for the model development.
Figure 6

A workflow diagram of this study.

Figure 6

A workflow diagram of this study.

Close modal
Figure 7 shows the input data, functions, and outcomes for the FOM. Users start by entering initial values to gather the required data for the model to work within FOM. Then, users can choose one of the five FOMs for operating the reservoir during floods. The results from FOM are divided into two types: common output, which covers the results from the selected FOM, and additional output, which includes results from calculations chosen by the user.
Figure 7

The model consists of user input, load data, selection of FOM, common output, and additional output.

Figure 7

The model consists of user input, load data, selection of FOM, common output, and additional output.

Close modal
Figure 8 shows the developed Graphical User Interface (interface) with reservoir characteristics and operational data for multipurpose reservoirs. The input data for the interface is 10-min or hourly inflow datasets. For example, when we input 10-min of inflow data, the model generates a reference graph every 10 min to support operators with flood operation decision-making. In the interface, users can input parameters (e.g., reservoir name, time interval, starting reservoir elevation, maximum reservoir elevation, inflow) and select the FOM.
Figure 8

Users can set input data for model operation and select the FOM within the interface.

Figure 8

Users can set input data for model operation and select the FOM within the interface.

Close modal

Case studies

We selected three significant flood events from 2010 (case study 1), 2011 (case study 2), and 2020 (case study 3) due to their severity and the availability of data at 10-min intervals. These events were analyzed to evaluate the applicability of the developed model and reference graph, ensuring they can effectively guide pre-release strategies for severe floods. By applying the model to these cases, we demonstrated its potential for practical use in flood management.

Input data

Input data includes reservoir characteristics, a table of storage by reservoir elevation, and a table of maximum release by reservoir elevation. Upon selecting the name of a multipurpose reservoir, the system internally retrieves the unique code of the reservoir and loads the data for the selected reservoir stored within the model. The Seomjingang reservoir has daily data from 1975, hourly data from 1992, and 10-min data from 2010. The developed model uses 10-min inflow data but can also accommodate hourly inflow data.

The discharge data for the flood events was provided by the Flood Control Office (https://www.hrfco.go.kr/river/resources01.do). The public can access 10-min release data through the Han River Flood Control Office (http://hrfco.go.kr/main.do). The unique codes of the reservoirs and historical hourly reservoir inflow data are available in the National Water Resources Management Information System (http://www.wamis.go.kr/) (Table 4). Input data for this article is publicly accessible (Yi & Yi 2024).

Table 4

A categorization of multipurpose reservoirs by basin, with unique codes assigned to each reservoir upon completion

BasinReservoir (reservoir unique code)
Han River Chungju (1003110), Hwengseung (1006110), Soyanggang (1012110) 
Nakdong River Andong (2001110), Bohyunsan (2012101), Gunwi (2008101), Gimcheon Buhang (2010101), Hapcheon (2015110), Imha (2002110), Milyang (2021110), Namgang (2018110), Seongdeok (2002111), Yeongju (2004101) 
Geum River Daecheong (3008110), Yongdam (3001110) 
West Coast of Geum River Boryeong (3203110) 
Mnkyung and Dongjin Buan (3303110) 
Seomjin River Juam (4007110), Seomjingang (4001110) 
Tamjin River Jangheung (5101110) 
BasinReservoir (reservoir unique code)
Han River Chungju (1003110), Hwengseung (1006110), Soyanggang (1012110) 
Nakdong River Andong (2001110), Bohyunsan (2012101), Gunwi (2008101), Gimcheon Buhang (2010101), Hapcheon (2015110), Imha (2002110), Milyang (2021110), Namgang (2018110), Seongdeok (2002111), Yeongju (2004101) 
Geum River Daecheong (3008110), Yongdam (3001110) 
West Coast of Geum River Boryeong (3203110) 
Mnkyung and Dongjin Buan (3303110) 
Seomjin River Juam (4007110), Seomjingang (4001110) 
Tamjin River Jangheung (5101110) 

Note. These codes are distinctive numbers used to load related data.

Load data

Based on user input, the model loads reservoir characteristics including low, restricted, normal high, flood, and maximum elevations. The table of storage by elevation lists the relation between storage volumes (MCM) and reservoir elevations (EL.m). Updated every 10 years following sedimentation surveys, this table is accessible on the Korea Water Resources Corporation (https://www.water.or.kr/). The table of maximum release by elevation contains maximum release based on the reservoir elevation, influenced by the location of spillways and their types.

Output data

The FOM model generates both common and additional outputs. The common outputs include reservoir operation results for the specified inflow period, such as releases, reservoir elevations, storage volumes, peak release, reference graph (peak release vs. target reservoir elevation) and a reference table. When users use functions 1 and 2 in FOM II, it produces the ratio as an additional output.

A reference graph is used to determine the target reservoir elevation after pre-release. This is a plot of the peak release on the x-axis and the target reservoir elevation on the y-axis. Once the reservoir elevation is reduced to the target elevation through pre-release, operators can make the corresponding peak release to make full use of the flood control storage. The following are the example steps for generating the reference graph and table for the Seomjingang reservoir. First, we run FOM V via an iterative process, using 100.0 CMS peak-release intervals as an example, to generate a series of target reservoir elevations after pre-releases. Second, we turn these results into the reference graph and table which are updated when new inflow forecasts become available. Third, peak release from the reservoir is determined by considering the downstream flood conditions. Fourth, from the reference graph, we read the target reservoir elevation (y-axis) using the peak release (x-axis). Fifth, pre-releases are made until the actual reservoir elevation reaches the designated target reservoir elevation. Finally, operators use the reference graph to adjust pre-releases based on the updating inflow forecasts and downstream flood conditions.

The final product is the reference graph and a corresponding reference table. The reference graph plots the peak release against the target reservoir elevation. We define the target reservoir elevation as the elevation after it has been lowered through pre-release, prior to starting flood operations. Flood control in real situations can be challenging for the reservoir operators as it requires urgent decision-making during the abrupt flood event.

We analyzed and presented the results for the Seomjingang reservoir using FOM V. The final outputs, including the reference graph and table, were generated at 100 CMS intervals through an iterative process. We analyzed three significant flood events from 2010 (case study 1), 2011 (case study 2), and 2020 (case study 3) for the Seomjingang reservoir and validated the model using the 2020 flood event in the Hapcheon reservoir.

Case study I

Application of FOM V for 2010 flood event

The case study I assessed the storm event from 15th to 17th August 2010 and the peak inflow was 3,500.0 CMS. The release was made less than the design release (1,810.0 CMS), yet the downstream area was still flooded (Figures 4(c) and 4(d)). The reservoir elevation was initially set at 188.6 EL.m on August 15th, 2010 with a design release. When the reservoir elevation was below the restricted water level (194.0 EL.m), the FOM V recommends the reservoir release the entire inflow up to the design release. Before the 2010 flood, the starting reservoir elevation was below the restricted water level (Figure 9). Because the reservoir elevation was low, we could not make the large release due to release capacity limitations. Instead, the reservoir stored the excess water (the difference between inflow and release), resulting in a reservoir elevation of 192.7 EL.m and a maximum release of 1,202.4 CMS. The results demonstrated more efficient operation using FOM V compared to the actual operation (Figure 4). However, the lateral inflow, in addition to the reservoir release, exacerbated the downstream flooding. From the results, we recommend reducing the release based on the downstream flood conditions, which can ultimately lead to better utilization of the available flood storage and reduce downstream damage.
Figure 9

Results for FOM V during the 2010 flood event: (a) inflow, release, and design release; (b) changes in reservoir elevation, restricted water level, and flood water level.

Figure 9

Results for FOM V during the 2010 flood event: (a) inflow, release, and design release; (b) changes in reservoir elevation, restricted water level, and flood water level.

Close modal

Application of reference graph for 2010 flood event

Once the operator sets the peak release at 500.0 CMS using the reference graph, they can store all inflow until the reservoir reaches 193.8 EL.m, at which point spillway gate releases can begin (Figure 10, Table 5). When the inflow hydrograph is updated, we re-evaluate and make decisions accordingly. Through this approach, the operators can utilize the flood control storage and reduce the peak release and the downstream flooding.
Table 5

A reference table corresponding to Figure 10 

Peak release (CMS)Target reservoir elevation (EL.m)Peak release (CMS)Target reservoir elevation (EL.m)
300.0 192.1 1,500.0 196.9 
400.0 193.0 1,600.0 197.1 
500.0 193.8 1,700.0 197.2 
600.0 194.4 1,800.0 197.3 
700.0 194.8 1,810.0 197.3 
800.0 195.3 1,900.0 197.3 
900.0 195.6 2,000.0 197.4 
1,000.0 195.9 2,100.0 197.5 
1,100.0 196.2 2,200.0 197.5 
1,200.0 196.4 2,300.0 197.6 
1,300.0 196.6 2,400.0 197.6 
1,400.0 196.8 2,500.0 197.7 
Peak release (CMS)Target reservoir elevation (EL.m)Peak release (CMS)Target reservoir elevation (EL.m)
300.0 192.1 1,500.0 196.9 
400.0 193.0 1,600.0 197.1 
500.0 193.8 1,700.0 197.2 
600.0 194.4 1,800.0 197.3 
700.0 194.8 1,810.0 197.3 
800.0 195.3 1,900.0 197.3 
900.0 195.6 2,000.0 197.4 
1,000.0 195.9 2,100.0 197.5 
1,100.0 196.2 2,200.0 197.5 
1,200.0 196.4 2,300.0 197.6 
1,300.0 196.6 2,400.0 197.6 
1,400.0 196.8 2,500.0 197.7 
Figure 10

A reference graph displays the relationship between the peak release and the target reservoir elevation for the 2010 flood event.

Figure 10

A reference graph displays the relationship between the peak release and the target reservoir elevation for the 2010 flood event.

Close modal

Case study II

Application of FOM V for 2011 flood event

Case study II evaluated the storm event from 8th to 11th August in 2011, which caused unprecedented streamflow in the Seomjin River Basin. The reservoir recorded a historic peak inflow (4,433.5 CMS) (Figures 11(a) and 11(b)). On 8th August, the starting elevation was 192.6 EL.m, and the peak release was at the design release (1,810.0 CMS). In FOM V, we released the same amount of inflow when the reservoir elevation was below the restricted water level and when the release was under the design release. During the severe storm starting around 12 PM on 9th August, the inflow surpassed the maximum release capacity. As a result, the reservoir elevation increased and eventually exceeded the restricted water level, requiring the flood control storage activation. However, the operator at that time did not fully utilize the entire flood control storage. Keeping the release below the design release would have allowed the operators to utilize more flood control storage, potentially reducing the impacts of flooding downstream.
Figure 11

Results for FOM V during the 2011 flood event: (a) inflow, release, and design release; (b) changes in reservoir elevation, restricted water level, and flood water level.

Figure 11

Results for FOM V during the 2011 flood event: (a) inflow, release, and design release; (b) changes in reservoir elevation, restricted water level, and flood water level.

Close modal

Application of reference graph for 2011 flood event

For the 2011 flood event, the reservoir elevation was kept low by making the design release (1,810.0 CMS). Once we reduced the release and stored the water in the flood control storage, we could have reduced the damage downstream. The operators can determine the target reservoir elevation after the pre-release based on the downstream flood conditions using a reference graph. For instance, if operators aim to keep the peak release below 700.0 CMS, they can use the reference graph to guide pre-release, lowering the reservoir elevation to below 193.0 EL.m (Figure 12, Table 6).
Table 6

A reference table corresponding to Figure 12 

Peak release (CMS)Target reservoir elevation (EL.m)Peak release (CMS)Target reservoir elevation (EL.m)
300.0 191.5 1,500.0 194.9 
400.0 192.0 1,600.0 195.1 
500.0 192.4 1,700.0 195.3 
600.0 192.7 1,800.0 195.5 
700.0 193.0 1,810.0 195.5 
800.0 193.3 1,900.0 195.6 
900.0 193.6 2,000.0 195.8 
1,000.0 193.8 2,100.0 195.9 
1,100.0 194.1 2,200.0 196.1 
1,200.0 194.3 2,300.0 196.2 
1,300.0 194.5 2,400.0 196.4 
1,400.0 194.7 2,500.0 196.5 
Peak release (CMS)Target reservoir elevation (EL.m)Peak release (CMS)Target reservoir elevation (EL.m)
300.0 191.5 1,500.0 194.9 
400.0 192.0 1,600.0 195.1 
500.0 192.4 1,700.0 195.3 
600.0 192.7 1,800.0 195.5 
700.0 193.0 1,810.0 195.5 
800.0 193.3 1,900.0 195.6 
900.0 193.6 2,000.0 195.8 
1,000.0 193.8 2,100.0 195.9 
1,100.0 194.1 2,200.0 196.1 
1,200.0 194.3 2,300.0 196.2 
1,300.0 194.5 2,400.0 196.4 
1,400.0 194.7 2,500.0 196.5 
Figure 12

A reference graph displays the relationship between the peak release and the target reservoir elevation for the 2011 flood event.

Figure 12

A reference graph displays the relationship between the peak release and the target reservoir elevation for the 2011 flood event.

Close modal

Case study III

Application of FOM V for 2020 flood event

The flood event from 7th to 9th August 2020, had a double-peak inflow that caused downstream flood damage (Figure 13). The reservoir started at a high reservoir elevation (193.5 EL.m) on 7th August due to a long-lasting storm with a peak release at the design release (1,810.0 CMS). Using FOM V, the reservoir released water at the design release for more than 24 h once the water level surpassed the restricted water level. Discharging at the design release for a long period caused downstream flooding. The reservoir did not fully utilize the flood control storage, suggesting room for releasing less than the design release. We tried to find a more effective approach to better make use of the flood control storage that could potentially reduce downstream flood risks.
Figure 13

Results for FOM V during the 2020 flood event: (a) inflow, release, and design release; (b) changes in reservoir elevation, restricted water level, and flood water level.

Figure 13

Results for FOM V during the 2020 flood event: (a) inflow, release, and design release; (b) changes in reservoir elevation, restricted water level, and flood water level.

Close modal

Application of reference graph for 2020 flood event

The 2020 floods showed that the peak release was the same as the design release, yet the flood control storage was not fully utilized, which was also observed during the 2011 flood. Considering the downstream flood conditions, it is preferable to make a smaller peak release while fully utilizing the flood control capacity. A reference graph was used to reduce downstream flood damage. For example, to maintain peak release under 1,000.0 CMS, operators can use the reference graph for pre-release guidance, aiming to reduce the reservoir elevation to below 192.6 EL.m (Figure 14, Table 7).
Table 7

A reference table corresponding to Figure 14 

Peak release (CMS)Target reservoir elevation (EL.m)Peak release (CMS)Target reservoir elevation (EL.m)
300.0 186.3 1,500.0 194.6 
400.0 187.7 1,600.0 195.0 
500.0 189.1 1,700.0 195.3 
600.0 190.0 1,800.0 195.6 
700.0 190.9 1,810.0 195.6 
800.0 191.5 1,900.0 195.8 
900.0 192.1 2,000.0 196.1 
1,000.0 192.6 2,100.0 196.3 
1,100.0 193.0 2,200.0 196.5 
1,200.0 193.5 2,300.0 196.7 
1,300.0 193.9 2,400.0 196.9 
1,400.0 194.3 2,500.0 197.1 
Peak release (CMS)Target reservoir elevation (EL.m)Peak release (CMS)Target reservoir elevation (EL.m)
300.0 186.3 1,500.0 194.6 
400.0 187.7 1,600.0 195.0 
500.0 189.1 1,700.0 195.3 
600.0 190.0 1,800.0 195.6 
700.0 190.9 1,810.0 195.6 
800.0 191.5 1,900.0 195.8 
900.0 192.1 2,000.0 196.1 
1,000.0 192.6 2,100.0 196.3 
1,100.0 193.0 2,200.0 196.5 
1,200.0 193.5 2,300.0 196.7 
1,300.0 193.9 2,400.0 196.9 
1,400.0 194.3 2,500.0 197.1 
Figure 14

A reference graph displays the relationship between the peak release and the target reservoir elevation for the 2020 flood event.

Figure 14

A reference graph displays the relationship between the peak release and the target reservoir elevation for the 2020 flood event.

Close modal

Application of FOM V for 2020 flood event (validation)

We selected the Hapcheon reservoir as a new site for model validation. The Hapcheon reservoir is a multipurpose reservoir located in the Nakdong River Basin. It supplies water to downstream areas and manages flood control using the FOM II method. Like the Seomjingang reservoir, the Hapcheon reservoir released a significant volume of water during the 2020 flood, causing severe flood damage in downstream regions. To validate the developed model, the 2020 flood event at the Hapcheon reservoir (7–9 August 2020) was selected for analysis.

We applied the FOM II method to operate the Hapchoen reservoir while maintaining a no-damage release volume of 500 CMS to prevent downstream damage. Figure 15 shows the flood season operation results for the Hapcheon reservoir. The reservoir was operated with a target reservoir elevation of 171.57 EL.m, and the fixed-rate parameter for FOM II was determined to be 18.01%.
Figure 15

Results for the Hapcheon reservoir with a maximum release of 500 CMS under FOM V during the 2020 flood event: (a) inflow and release; (b) changes in reservoir elevation, restricted water level, and flood water level.

Figure 15

Results for the Hapcheon reservoir with a maximum release of 500 CMS under FOM V during the 2020 flood event: (a) inflow and release; (b) changes in reservoir elevation, restricted water level, and flood water level.

Close modal
Figure 16 is a reference graph generated by applying FOM II to the 2020 flood event. To prevent downstream damage and keep release volumes below 500 CMS, the initial water level (target reservoir elevation) must be less than 171.57 EL.m. Considering the current reservoir water level is 175.26 EL.m, the graph indicates that additional pre-release is required to achieve a release volume of 500 CMS using the FOM II method.
Figure 16

A reference graph displays the relationship between the peak release and the target reservoir elevation for the 2020 flood event in the Hapcheon reservoir.

Figure 16

A reference graph displays the relationship between the peak release and the target reservoir elevation for the 2020 flood event in the Hapcheon reservoir.

Close modal

We developed a reservoir operation model to guide operators in reducing peak releases from reservoirs during the flood season. The model generates reference tables and graphs through an iterative process to determine the target reservoir elevation after pre-release and offers a practical application for prompt decision-making in real-time reservoir operations. Once operators identify the target reservoir elevation, they initiate pre-release operations until the desired elevation is reached. The newly developed model guides operators in determining the target reservoir elevation for pre-release by incorporating forecasted inflow and downstream flood conditions.

The developed reservoir simulation model can run five FOMs. We used the historical inflow data of 2010, 2011, and 2020 from the Seomjingang reservoir to demonstrate developing the reference graph and table using FOM V. These final products were used to determine the target reservoir elevation to ensure that the peak release does not exceed the design release while taking the downstream flood conditions into account. Once operators determine the target reservoir elevation, they start the pre-release until they reach that elevation before beginning flood operations. When updated forecasted inflow data become available, such as every 10-min, the model recalculates the target reservoir elevation. Based on this new information, we then adjust the release accordingly. Overforecasting the inflow could lead to excessive pre-release, lowering reservoir levels too much and risking the water supply during subsequent dry periods. This approach offers real-time decision-making that allows for proactive reservoir operation, helping to reduce the downstream flood damage and ensuring an adequate water supply for the upcoming dry season.

This study has several limitations and areas for future improvement. One limitation is the lack of consideration for flow routing from the reservoir to the downstream control point, as the downstream flow was monitored at a water level station. However, in cases where no monitoring stations are available downstream, incorporating flow routing becomes essential. Additionally, uncertainties in this study stem from the accuracy of inflow forecasting and the exclusion of the time required to open and close spillway gates, which could impact real-time applicability (Kim et al. 2018). Future research should focus on incorporating flow routing to better capture the dynamics of reservoir releases reaching the control point. Furthermore, developing a new FOM is essential, as different FOMs can lead to varying levels of downstream damage from the same flood event.

The effectiveness of the pre-release varies significantly across different factors such as peak inflows, spillway release capacities, locations, downstream design flood, reservoirs, and basin characteristics. One of the uncertainties in the pre-release strategy comes from unreliable meteorological and hydrological forecasting. When these forecasts inaccurately predict the storm events, the reservoir release may be underestimated or overestimated. Future research includes obtaining reliable forecasting data as early as possible prior to a flood event.

Flood control during actual flood events poses challenges for reservoir operators due to the need for rapid decision-making. We developed an approach that provides operators with a tool for making prompt operation decisions to better protect downstream regions from flooding and prevent dam failure during storm events. This study not only improves how reservoirs are managed during the flood event but also contributes to broader discussions on flood management, marking a shift towards more secure, efficient, and flexible reservoir operation strategies.

This research received no specific grant from any funding agency in the public, commercial, or not-for-profit sectors.

E.L. conceptualized the study, conducted data curation, formal analysis, investigation, methodology development, and resource management, and also handled project administration, software development, validation, visualization, writing of the original draft, and review and editing of the article. S.Y. contributed to resources, visualization, writing of the original draft, and review and editing of the article. J.J. was responsible for methodology, resources, software, and also took part in the review and editing of the article. J.H. handled software and participated in the review and editing of the article. S.L. contributed to resources and the review and editing of the article. J.Y. managed resources and participated in the review and editing of the article. J.Y. was involved in the conceptualization, methodology, project administration, resources, software, supervision, writing of the original draft, and review and editing of the article.

All relevant data are included in the paper or its Supplementary Information.

The authors declare there is no conflict.

Alfieri
L.
,
Bisselink
B.
,
Dottori
F.
,
Naumann
G.
,
de Roo
A.
,
Salamon
P.
,
Wyser
K.
&
Feyen
L.
(
2017
)
Global projections of river flood risk in a warmer world
,
Earth's Future
,
5
(
2
),
171
182
.
https://doi.org/10.1002/2016EF000485
.
Beven
K.
(
1993
)
Prophecy, reality and uncertainty in distributed hydrological modelling
,
Advances in Water Resources
,
16
(
1
),
41
51
.
https://doi.org/10.1016/0309-1708(93)90028-E
.
Celeste
A. B.
&
Billib
M.
(
2009
)
Evaluation of stochastic reservoir operation optimization models
,
Advances in Water Resources
,
32
(
9
),
1429
1443
.
https://doi.org/10.1016/j.advwatres.2009.06.008
.
Chaves
P.
&
Chang
F.-J.
(
2008
)
Intelligent reservoir operation system based on evolving artificial neural networks
,
Advances in Water Resources
,
31
(
6
),
926
936
.
https://doi.org/10.1016/j.advwatres.2008.03.002
.
Chen
J.
,
Guo
S.
,
Li
Y.
,
Liu
P.
&
Zhou
Y.
(
2013
)
Joint operation and dynamic control of flood limiting water levels for cascade reservoirs
,
Water Resources Management
,
27
(
3
),
749
763
.
https://doi.org/10.1007/s11269-012-0213-z
.
Chen
H.
,
Constante-Flores
G. E.
&
Li
C.
(
2024
)
Diagnosing infeasible optimization problems using large language models
,
INFOR: Information Systems and Operational Research
,
62
(
4
),
573
587
.
https://doi.org/10.1080/03155986.2024.2385189
.
Cheng
C.
&
Chau
K. W.
(
2001
)
Fuzzy iteration methodology for reservoir flood control operation
,
Journal of the American Water Resources Association
,
37
(
5
),
1381
1388
.
https://doi.org/10.1111/j.1752-1688.2001.tb03646.x
.
Chou
F. N.-F.
&
Wu
C.-W.
(
2013
)
Expected shortage based pre-release strategy for reservoir flood control
,
Journal of Hydrology
,
497
,
1
14
.
https://doi.org/10.1016/j.jhydrol.2013.05.039
.
Dobson
B.
,
Wagener
T.
&
Pianosi
F.
(
2019
)
An argument-driven classification and comparison of reservoir operation optimization methods
,
Advances in Water Resources
,
128
,
74
86
.
https://doi.org/10.1016/j.advwatres.2019.04.012
.
Endo
A.
,
Yamada
M.
,
Miyashita
Y.
,
Sugimoto
R.
,
Ishii
A.
,
Nishijima
J.
,
Fujii
M.
,
Kato
T.
,
Hamamoto
H.
,
Kimura
M.
,
Kumazawa
T.
&
Qi
J.
(
2020
)
Dynamics of water–energy–food nexus methodology, methods, and tools
.
Current Opinion in Environmental Science and Health
,
13
,
46
60
.
https://doi.org/10.1016/j.coesh.2019.10.004
.
Ghobadi
M.
&
Kaboli
H. S.
(
2020
)
Developing a Web-based decision support system for reservoir flood management
,
Journal of Hydroinformatics
,
22
(
3
),
641
662
.
https://doi.org/10.2166/hydro.2020.185
.
Hidayah Ishak
N.
&
Mustafa Hashim
A.
(
2018
)
Dam pre-release as an important operation strategy in reducing flood impact in Malaysia
,
E3S Web of Conferences
,
34
,
02017
.
https://doi.org/10.1051/e3sconf/20183402017
.
Hossain
M. S.
,
Nair
M.
,
Mohd Sidek
L.
&
Marufuzzaman
M.
(
2020
)
A Pre-release Concept for Reservoir Management and the Effect Analysis on Flood Control
. In: Mohd Sidek, L., Salih, G., Boosroh, M. (eds)
ICDSME 2019. ICDSME 2019. Water Resources Development and Management
.
Springer, Singapore. https://doi.org/10.1007/978-981-15-1971-0_54
.
Huang
C.
,
Li
W.
,
He
S.
&
Yang
Y.
(
2024
)
Development and application of reservoir operation method based on pre-release index for control of exceedance floods
,
Water
,
16
(
22
),
3229
.
https://doi.org/10.3390/w16223229
.
Jain
S. K.
,
Yoganarasimhan
G. N.
&
Seth
S. M.
(
1992
)
A risk-based approach for flood control operation of a multipurpose reservoir
,
Journal of the American Water Resources Association
,
28
(
6
),
1037
1043
.
https://doi.org/10.1111/j.1752-1688.1992.tb04015.x
.
Jiang
Y.
,
Zhang
R.
&
Wang
B.
(
2022
)
Scenario-based approach for emergency operational response: implications for reservoir management decisions
,
International Journal of Disaster Risk Reduction
,
80
,
103192
.
https://doi.org/10.1016/j.ijdrr.2022.103192
.
Karaboga
D.
,
Bagis
A.
&
Haktanir
T.
(
2008
)
Controlling spillway gates of dams by using fuzzy logic controller with optimum rule number
,
Applied Soft Computing
,
8
(
1
),
232
238
.
https://doi.org/10.1016/j.asoc.2007.01.004
.
Kim
S.-H.
,
Kang
S.-U.
&
Bae
D.-H.
(
2018
)
Uncertainty assessment of ensemble stream ow prediction method
,
Journal of Korea Water Resources Association
,
51
(
6
),
5
6
.
Kim
Y.-G.
,
Jo
M.-B.
,
Kim
P.
,
Oh
S.-N.
,
Paek
C.-H.
&
So
S.-R.
(
2021
)
Effective optimization-simulation model for flood control of cascade barrage network
,
Water Resources Management
,
35
(
1
),
135
157
.
https://doi.org/10.1007/s11269-020-02715-0
.
Krzysztofowicz
R.
&
Duckstein
L.
(
1979
)
Preference criterion for flood control under uncertainty
,
Water Resources Research
,
15
(
3
),
513
520
.
https://doi.org/10.1029/WR015i003p00513
.
Lee
E.
,
Ji
J.
,
Lee
S.
,
Yoon
J.
,
Yi
S.
&
Yi
J.
(
2023a
)
Development of an optimal water allocation model for reservoir system operation
,
Water
,
15
(
20
),
3555
.
https://doi.org/10.3390/w15203555
.
Lee
S.
,
Choi
Y.
,
Ji
J.
,
Lee
E.
,
Yi
S.
&
Yi
J.
(
2023b
)
Flood vulnerability assessment of an urban area: a case study in Seoul, South Korea,
,
Water
,
15
(
11
),
1–21. https://doi.org/10.3390/w15111979
.
Li
X.
,
Guo
S.
,
Liu
P.
&
Chen
G.
(
2010
)
Dynamic control of flood limited water level for reservoir operation by considering inflow uncertainty
,
Journal of Hydrology
,
391
(
1–2
),
124
132
.
https://doi.org/10.1016/j.jhydrol.2010.07.011
.
Liu
P.
,
Guo
S.
,
Xiong
L.
,
Li
W.
&
Zhang
H.
(
2006
)
Deriving reservoir refill operating rules by using the proposed DPNS model
,
Water Resources Management
,
20
(
3
),
337
357
.
https://doi.org/10.1007/s11269-006-0322-7
.
Liu
Y.
,
Hou
G.
,
Wang
B.
,
Xu
Y.
,
Tian
R.
,
Wang
T.
&
Qin
H.
(
2024
)
Many-objective hierarchical pre-release flood operation rule considering forecast uncertainty
,
Water
,
16
(
5
),
785
.
https://doi.org/10.3390/w16050785
.
Lu
Q.
,
Zhong
P.
,
Xu
B.
,
Huang
X.
,
Zhu
F.
,
Wang
H.
&
Ma
Y.
(
2022
)
Multi-objective risk analysis for flood control operation of a complex reservoir system under multiple time-space correlated uncertainties
,
Journal of Hydrology
,
606
,
127419
.
https://doi.org/10.1016/j.jhydrol.2021.127419
.
Mediero
L.
,
Garrote
L.
&
Martin-Carrasco
F.
(
2007
)
A probabilistic model to support reservoir operation decisions during flash floods
,
Hydrological Sciences Journal
,
52
(
3
),
523
537
.
https://doi.org/10.1623/hysj.52.3.523
.
Meng
X.
&
Wu
X. B.
(
2013
)
Study on flood control pre-discharge dispatching scheme of reservoir based on fuzzy optimum selection
,
Applied Mechanics and Materials
,
353–356
,
2641
2644
.
https://doi.org/10.4028/www.scientific.net/AMM.353-356.2641
.
Nguyen
T. H.
,
Gourbesville
P.
,
Vo
N. D.
&
Vo
N. D. P.
(
2020
)
Pre-release strategy for ood control in the multi-reservoir and rivers system
. In: Gourbesville, P., Caignaert, G. (eds)
Advances in Hydroinformatics
.
Springer
, pp.
409
416
.
https://doi.org/10.1007/978-981-15-5436-0_32
.
Rezay Nazarzadeh
M.
,
AkhondAli
A.
&
Daneshkhah
A.
(
2020
)
Optimization of reservoir operation for real-time flood control with emphasis on forecast uncertainty: a case study of dez reservoir
,
Journal of Hydraulic Structures
,
6
(
3
),
92
107
.
https://doi.org/10.22055/jhs.2021.34694.1146
.
Wei
G.
,
Tych
W.
,
Beven
K.
,
He
B.
,
Ning
F.
&
Zhou
H.
(
2018
)
Nierji reservoir flood forecasting based on a data-based mechanistic methodology
,
Journal of Hydrology
,
567
,
227
237
.
https://doi.org/10.1016/j.jhydrol.2018.10.026
.
Wei
G.
,
Liang
G.
,
Ding
W.
,
He
B.
,
Wu
J.
,
Ren
M.
&
Zhou
H.
(
2022
)
Deriving optimal operating rules for flood control considering pre-release based on forecast information
,
Journal of Hydrology
,
615
,
128665
.
https://doi.org/10.1016/j.jhydrol.2022.128665
.
Yi
S.
&
Yi
J.
(
2024
)
Reservoir-based flood forecasting and warning: deep learning versus machine learning
,
Applied Water Science
,
14
,
237
.
https://doi.org/10.1007/s13201-024-02298-w
.
This is an Open Access article distributed under the terms of the Creative Commons Attribution Licence (CC BY-ND 4.0), which permits copying and redistribution with no derivatives, provided the original work is properly cited (http://creativecommons.org/licenses/by-nd/4.0/).