The research of joint optimization operation of complex flood control systems is still in the process of development. This paper introduces a decomposition–coordination model for solving the multi-objective optimization problem for real-time flood control operation in reservoir group and flood storage basin. The multi-objective programming is established for maximum safety of the reservoir group and minimum losses of flood storage basin, according to the real-time flood control requirements. Then, a third-order hierarchical optimization decomposition–coordination model is proposed for solving the multi-objective programming problem, based on the decomposition–coordination principle of large scale system theory. It takes advantage of an objective coordination method and model coordination method to accomplish global optimization and combines progressive optimality algorithm to solve the subsystem local optimization. Finally, the model is applied for simulating the storm flood in July 2007 in the middle reaches of the Huaihe River Basin in China. Results show that the proposed decomposition–coordination model can efficiently calculate the reservoir group optima release strategy and flood storage basin diversion process, and meet the safety discharge at the downstream control section.

## INTRODUCTION

In China, flood disasters cause massive economic losses and casualties, and have a higher ranking in impact than other natural disasters. Reservoirs are the most effective water storage facilities to control floods. As well, flood storage basins, such as low-lying farming areas and large lakes, have been exploited as temporary and auxiliary water storage projects when extreme floods are beyond the water storage capacity of reservoirs. As a result, the critical question arises of how to scientifically and rationally use various engineering facilities to control floods?

Many mathematical models and calculation methods have been applied to solve the problem. Windsor (1973) first initiated a linear programming (LP) model for application in reservoir flood control operation. Yakowitz (1982) formulated a dynamic programming (DP) model for application in water resources. Unver & Mays (1990) used a nonlinear programming (NLP) model for real-time hourly flood control problems in flood-prone areas, with the model taking the minimum total flood damage as its objective function. Karbowski *et al*. (2005) developed a hybrid analytic/rule-based approach for real-time flood control operation of a single reservoir. Wei & Hsu (2008) used a balanced water level index method to determine the highest release priority in reservoirs, and the method was applied in estimating real-time release in two parallel reservoirs during floods. Zhong *et al*. (2010) presented an excess-water distribution model for real-time flood control operation in a reservoir group; a dynamic adjustment index was proposed in the model to determine the release priority, and the objective function was to minimize the maximum discharge at a downstream control section. Moreover, many new theories and methods have been introduced into the reservoir optimization operation which have enriched the research methods of reservoir joint operation, such as genetic algorithm (GA) (e.g., Chang & Chen 1998; Chang 2008), fuzzy method (e.g., Cheng & Chau 2001; Fu 2008), particle swarm optimization (PSO) (e.g., Janga Reddy & Nagesh Kumar 2007), artificial neural network (ANN) (e.g., Chandramouli & Raman 2001; EI-Shafie & EI-Manadely 2011), and other real-time models (e.g., Hsu & Wei 2007; Huang & Hsieh 2010; Richaud *et al*. 2011), and uncertainty (e.g., Brandimarte & Di Baldassarre 2012). However, few studies have focused on the joint operation problem of flood storage basin (e.g., Wang *et al*. 2009; Liu *et al*. 2010), especially for real-time flood control optimal operation.

All these studies have successfully solved the corresponding reservoir operation problem in detail. The method depends on the characteristics of the reservoir system. However, the use of a single method has been limited, even not applicable, as reservoir systems increase. At the same time, the method for joint optimal operation for a complex flood control system is still in the process of development.

The decomposition–coordination method of large scale system theory (e.g., Mesarovic 1970; Singhand & Titli 1978; Li *et al*. 2007) can divide a large scale system into several independent subsystems, for which, the coordinators are installed to form hierarchical structure. The subsystems do local optima under some interference information coming from coordinators, and then send feedback to coordinators. The coordinators are responsible for coordinating based on the objective function to achieve the global optimum. The decomposition–coordination method has two significant advantages: the optimization order among each subsystem is arbitrary and the optimization method in each subsystem can be different; the method can reduce system dimensions and save computing time. Thus, it can be explored to analyze and solve the real-time flood control problem for joint operation in a reservoir group and flood storage basin, which has large scale, multi-objective, multi-constraint, non-linear and dynamic characteristics.

In this paper, a third-order hierarchical optimization decomposition–coordination model is introduced to solve the multi-objective optimization problem for real-time flood control operation in a reservoir group and flood storage basin. We seek here to: (1) describe the flood control problem by establishing multi-objective programming; (2) coordinate for global optima in coordinators using an objective coordination method and model coordination method, and calculate for local optima in subsystems using progressive optimality algorithm (POA) (e.g., Howson & Sancho 1975; Simonovic 1979; Turgeon 1981); and (3) apply the decomposition–coordination model for real-time flood control operation.

## METHODOLOGY

In this section, we propose a methodology for solving a certain joint flood control operation problem in reservoir group and flood storage basin.

The method includes three processes, as follows. (1) Multi-objective programming: for the mathematical description of real-time flood control problem. (2) Decomposition–coordination model: according to the feature of spatial structure of the multi-objective programming, a corresponding decomposition and coordination method are adopted to establish a decomposition–coordination model. The model contains hierarchical structure, components and calculation methods. (3) Procedures of real-time operation: the calculation process for running the decomposition–coordination model.

In the following sections, we describe the three parts in detail.

### Multi-objective programming

A flood control system is a complex connected system, which generally consists of reservoir group, rivers, flood storage basin, and other engineering components. For flood control, the reservoir group changes outflow through the modulation of inflow to effectively reduce the flow peak and flood volume at downstream control section. Rivers attenuate flood waves through river storage. Flood storage basin is the temporary storage place for overflow flood when the flood cannot be fully controlled by the reservoir group and rivers. For a flood control system, the joint optimization operation should meet four objectives: (1) ensuring dam safety; (2) meeting terminal water storage for reservoir; (3) guaranteeing safety discharge in rivers; and (4) minimizing flood diversion losses in the flood storage basin. The second objective and the third objective are satisfied by constraints Equations (8) and (13). The first objective and the fourth objective are considered in the objective functions. Thus, the multi-objective programming is described as follows.

#### Objective functions

*i*th reservoir safety;

*n*is the number of reservoirs; is the

*i*th reservoir flood control capacity which has been used before operating; is the

*i*th reservoir design flood control capacity; and are inflow and outflow of the

*i*th reservoir; is the time interval;

*T*is the length of operation period.

*i*th flood storage basin losses;

*m*is the number of flood storage basins.

*i*th flood storage basin; is the initial flood storage amount of the

*i*th flood storage basin; is the flood storage process of the

*i*th flood storage basin; , are the coefficients of cubic polynomial.

In Equation (6), and are unknown variables, the other variables are constants, and the equation satisfies the linear superposition. Obviously, the objectives and are competing with each other, the determination of the weighting coefficients and depends on the decision-makers, thus, we can develop a series of analysis schemes for supporting the decision-makers to make the final decisions.

#### Constraints

##### Constraints of reservoir

##### Constraints of rivers

*i*th reservoir outflow process and the

*i*th flood storage basin diversion, respectively; is the interval flood process; is safety discharge at control section.

##### Constraints of flood storage basin

In addition, all the decision variables are non-negative constraints.

### Decomposition–coordination model

The proposed multi-objective programming is difficult for directly calculating by a single method in mathematic. However, the programming issue meets the (two levels) original cubic triangle structure (refers to Mesarovic (1970) and Singhand & Titli (1978)) seen from spatial distribution. Thus, it can be solved by a decomposition and coordination method of large scale system theory. The key step for applying this method is decoupling (relieve the coupling constraints), then, hierarchical structure and coordination approach are formed. This section includes two parts: (1) third-order hierarchical structure for the decomposition and coordination information after two levels decoupling; (2) components and calculation methods including three coordination models and corresponding coordination methods, two local optimization models, and corresponding calculation methods.

#### Third-order hierarchical structure

*Reservoir group subsystem coordination model*and

*Flood storage basin subsystem coordination model*). Finally, a third-order hierarchical structure is shown in Figure 1.

#### Components and calculation methods

##### Large scale system coordination model

*k*is the number of iterations; is the

*k*th computation step.

##### Reservoir group subsystem coordination model

*k*is the number of iterations; is the

*k*th computation step.

If iteration in the reservoir group subsystem coordination layer meets the condition (where is iteration accuracy), it may be concluded that the reservoir group subsystem objective function reaches optimization and the iteration calculation should be stopped.

##### Flood storage basin subsystem coordination model

*k*is the number of iterations; is the

*k*th computation step.

If iteration in flood storage basin subsystem coordination layer meets the condition (where is iteration accuracy), it may be concluded that the flood storage basin subsystem objective function has reached optimization and the iteration calculation should be stopped.

##### Single reservoir operation

*i*th reservoir is shown in Equation (28). The constraints for reservoir operation are Equations (7)–(11). The optimal operation belongs to a multi-stage decision problem, where stage variable is time

*t*, decision variable is the

*i*th reservoir outflow . Considering and can meet Equation (12), namely, , the solution for single reservoir optimal problem has backward effectiveness and the POA can be used to solve this problem.

##### Single flood storage basin operation

The constraints for flood storage basin operation are Equations (14)–(16). As and meet Equation (12), that is, , the solution for single flood storage basin optimal problem has backward effectiveness and POA can be used to solve this problem. In the case study, we can ignore Equation (12), that is, , due to the small distance between flood storage basin and control section. The backward effectiveness problem does not exist at this time, and other methods, such as dynamic programming (DP) method, can be used to solve this problem.

### Procedures of real-time operation

Step 1: Start real-time operation analysis.

Step 2: Receive and renew the latest hydrological observed information and hydrological forecasting information at current time, including start water level at current time in reservoir, reservoir inflow process , interval flood process , initial water volume at current time in flood storage basin, and water level at current time at downstream control section.

Step 3: Input decision control information including weighting coefficients

*α*and_{R}*α*(by decision-makers), the length of time period_{D}*T*, time interval Δ*t*, flood routing coefficients , , , safety discharge at control section, the various control water levels and releases (, , , , ) in reservoir, the design diversion flow , the design storage volume , and fitting coefficients (, , , ) in flood storage basin.Step 4: Apply the decomposition–coordination model for real-time operation in reservoir group and flood storage basin.

- Step 5: Given the initial values of and , a recommended approach is described as: (1) calculate the excess flood process in natural state (without reservoir group and flood storage basin operation) at control section, denoted as . Thus, where is the response process at control section from the
*i*th reservoir inflow ; (2) calculate the initial variables, where and . Step 7: Call the POA calculation module to do local optimization,

*n*reservoirs are calculated separately (as seen in the section*Single reservoir operation*).Step 8: Judge the convergence criteria in reservoir group (as seen in the section

*Reservoir group subsystem coordination model*). If the convergence criteria are satisfied, then continue the calculation; otherwise, renew the coordinating information , then return to step 7.Step 10: Call the POA or DP calculation module to do local optimization,

*m*flood storage basins are calculated separately (as seen in section*Single flood storage basin operation*).Step 11: Judge the convergence criteria in flood storage basin (as seen in the section

*Flood storage basin subsystem coordination model*). If the convergence criteria are satisfied, then continue the calculation; otherwise, renew the coordinating information , then return to step 10.Step 12: Judge the convergence criteria in large scale system (as seen in the section

*Large scale system coordination model*). If the convergence criteria are satisfied, then continue the calculation; otherwise, renew the coordinating information , then return to step 6.Step 13: Output the optimal calculation results including the optimal release process in each reservoir, the optimal diversion process in each flood storage basin, and the final flow synthesis process at downstream control section.

Step 14: End real-time operation analysis.

** Notes**: The proposed calculation procedures are implemented by the support of computer programming language (Visual Basic 6.0) and database technology (SQL 2008). The initial values of , , , and will directly influence the calculation speed and convergence quality, which deserves further study. In this paper, an approach for determining the initial values of the four variables is given for a reference.

## STUDY AREA AND DATA

Huaihe River Basin, located between the Yangtze River and Yellow River in China, belongs to a warm temperate semi-humid monsoon climate zone and has continental climate characteristics. Large reservoirs and flood storage basin projects above the Lutaizi station are distributed from upstream to downstream, and can be considered as a complex joint flood control system with reservoirs, rivers, and flood storage basins.

Figure 3 shows the location of the main reservoirs and flood storage basins in the middle reaches of Huaihe River Basin, where Lutaizi is the control section. In the upstream, there are four large reservoirs, Nianyushan, Meishan, Xianghongdian, and Fozilin, and three important flood storage basins near the control section, Qiujia Lake, Jiangtan Lake and Chengdong Lake, and also three main tributaries, the Ying River, Shi-guan River, and Pi River.

The flood in July 2007 is used as the case study. The inflow flood process of four reservoirs, interval flood process between reservoirs and Lutaizi, flood process at Lutaizi and each river flood routing parameters are known. The safety discharge at Lutaizi control section is 7,500 m^{3}/s, and the time interval is 3 h.

The proposed decomposition–coordination model in the reservoir group and flood storage basin was used for joint flood control. Reservoir group and flood storage basin operating control parameters are shown in Tables 1 and 2. The flood routing is not considered as the three flood storage basins are close to Lutaizi control section. Downstream flood routing parameters of the four reservoirs are shown in Table 3.

Reservoirs . | Start water level . | Terminal water level . | Lowest water level . | Highest water level . | The minimum discharge . | Outflow allowable amplitude . |
---|---|---|---|---|---|---|

Nianyushan | 106.3 | 106.5 | 105.8 | 114.5 | 60 | 1,000 |

Meishan | 128.8 | 129.0 | 125.3 | 137.7 | 100 | 1,000 |

Xianghongdian | 131.2 | 131.5 | 123.0 | 141.0 | 100 | 1,000 |

Fozilin | 117.8 | 117.8 | 117.6 | 125.7 | 20 | 1,000 |

Reservoirs . | Start water level . | Terminal water level . | Lowest water level . | Highest water level . | The minimum discharge . | Outflow allowable amplitude . |
---|---|---|---|---|---|---|

Nianyushan | 106.3 | 106.5 | 105.8 | 114.5 | 60 | 1,000 |

Meishan | 128.8 | 129.0 | 125.3 | 137.7 | 100 | 1,000 |

Xianghongdian | 131.2 | 131.5 | 123.0 | 141.0 | 100 | 1,000 |

Fozilin | 117.8 | 117.8 | 117.6 | 125.7 | 20 | 1,000 |

Flood storage . | Initial water volume . | Design storage capacity . | Design diversion flow . | Fitting coefficient . | |||
---|---|---|---|---|---|---|---|

basins . | . | . | . | . | . | . | . |

Qiujia Lake | 86 | 194 | 1,200 | 1.05 | − 7.3019 | 16.5970 | − 5.3486 |

Jiangtang Lake | 324 | 860 | 3,400 | 0.23 | − 0.3572 | 0.7553 | − 0.0577 |

Chengdong Lake | 628 | 1,590 | 1,800 | 1.51 | − 1.5522 | 0.4919 | − 0.0187 |

Flood storage . | Initial water volume . | Design storage capacity . | Design diversion flow . | Fitting coefficient . | |||
---|---|---|---|---|---|---|---|

basins . | . | . | . | . | . | . | . |

Qiujia Lake | 86 | 194 | 1,200 | 1.05 | − 7.3019 | 16.5970 | − 5.3486 |

Jiangtang Lake | 324 | 860 | 3,400 | 0.23 | − 0.3572 | 0.7553 | − 0.0577 |

Chengdong Lake | 628 | 1,590 | 1,800 | 1.51 | − 1.5522 | 0.4919 | − 0.0187 |

Items . | C0
. _{i} | C1
. _{i} | C2
. _{i} | Nianyushan to Lutaizi . | Meishan to Lutaizi . | Xianghongdian to Lutaizi . | Fozilin to Lutaizi . |
---|---|---|---|---|---|---|---|

Parameters/Reach numbers | 0.2 | 0.6 | 0.2 | 18 | 17 | 15 | 15 |

Items . | C0
. _{i} | C1
. _{i} | C2
. _{i} | Nianyushan to Lutaizi . | Meishan to Lutaizi . | Xianghongdian to Lutaizi . | Fozilin to Lutaizi . |
---|---|---|---|---|---|---|---|

Parameters/Reach numbers | 0.2 | 0.6 | 0.2 | 18 | 17 | 15 | 15 |

## RESULTS AND DISCUSSION

. | . | Reservoir safety . | Reservoir group . | Flood storage basin losses . | Flood storage . | Total . | Large scale . | |||||
---|---|---|---|---|---|---|---|---|---|---|---|---|

Program number . | Weight distribution . | Nianyushan . | Meishan . | Xianghongdian . | Fozilin . | subsystem safety . | Qiujia Lake . | Jiangtan Lake . | Chengdong Lake . | basin subsystem losses . | diversion/10^{6}m^{3}
. | system target value . |

1 | 0,1 | 0.76 | 0.67 | 0.56 | 0.91 | 2.90 | 0 | 0 | 0 | 0 | 0 | 0 |

2 | 0.1,0.9 | 0.76 | 0.67 | 0.56 | 0.91 | 2.90 | 0 | 0 | 0 | 0 | 0 | −0.0725 |

3 | 0.2,0.8 | 0.76 | 0.67 | 0.56 | 0.91 | 2.90 | 0 | 0 | 0 | 0 | 0 | −0.1450 |

4 | 0.3,0.7 | 0.76 | 0.67 | 0.56 | 0.91 | 2.90 | 0 | 0 | 0 | 0 | 0 | −0.2175 |

5 | 0.4,0.6 | 0.76 | 0.67 | 0.56 | 0.91 | 2.90 | 0 | 0 | 0 | 0 | 0 | −0.2900 |

6 | 0.5,0.5 | 0.76 | 0.67 | 0.56 | 0.91 | 2.90 | 0 | 0 | 0 | 0 | 0 | −0.3625 |

7 | 0.51,0.49 | 0.760 | 0.670 | 0.560 | 0.910 | 2.900 | 0 | 0 | 0 | 0 | 0 | −0.3698 |

8 | 0.52,0.48 | 0.760 | 0.670 | 0.560 | 0.910 | 2.900 | 0 | 0 | 0 | 0 | 0 | −0.3770 |

9 | 0.53,0.47 | 0.762 | 0.672 | 0.562 | 0.912 | 2.908 | 3.65 | 0 | 0 | 3.65 | 0.11 | −0.3527 |

10 | 0.54,0.46 | 0.764 | 0.674 | 0.564 | 0.914 | 2.916 | 3.81 | 0 | 0 | 3.81 | 1.78 | −0.3604 |

11 | 0.55,0.45 | 0.766 | 0.676 | 0.566 | 0.915 | 2.923 | 3.97 | 0 | 0 | 3.97 | 3.47 | −0.3680 |

12 | 0.56,0.44 | 0.768 | 0.678 | 0.567 | 0.917 | 2.930 | 4.13 | 0 | 0 | 4.13 | 5.15 | −0.3757 |

13 | 0.57,0.43 | 0.770 | 0.680 | 0.569 | 0.919 | 2.938 | 4.29 | 0 | 0 | 4.29 | 6.80 | −0.3836 |

14 | 0.58,0.42 | 0.771 | 0.682 | 0.571 | 0.921 | 2.945 | 4.45 | 0 | 0 | 4.45 | 8.42 | −0.3915 |

15 | 0.59,0.41 | 0.773 | 0.684 | 0.573 | 0.923 | 2.953 | 4.61 | 0 | 0 | 4.61 | 10.08 | −0.3997 |

16 | 0.6,0.4 | 0.77 | 0.69 | 0.58 | 0.92 | 2.96 | 4.77 | 0 | 0 | 4.77 | 11.68 | −0.4078 |

17 | 0.7,0.3 | 0.78 | 0.71 | 0.59 | 0.94 | 3.02 | 5.89 | 0 | 0 | 5.89 | 23.06 | −0.4949 |

18 | 0.8,0.2 | 0.80 | 0.72 | 0.61 | 0.95 | 3.08 | 7.02 | 0 | 0 | 7.02 | 34.83 | −0.5893 |

19 | 0.9,0.1 | 0.82 | 0.73 | 0.62 | 0.97 | 3.14 | 8.14 | 0 | 0 | 8.14 | 47.35 | −0.6910 |

20 | 1,0 | 0.84 | 0.74 | 0.63 | 0.98 | 3.19 | 9.26 | 0 | 0 | 9.26 | 62.06 | −0.7975 |

. | . | Reservoir safety . | Reservoir group . | Flood storage basin losses . | Flood storage . | Total . | Large scale . | |||||
---|---|---|---|---|---|---|---|---|---|---|---|---|

Program number . | Weight distribution . | Nianyushan . | Meishan . | Xianghongdian . | Fozilin . | subsystem safety . | Qiujia Lake . | Jiangtan Lake . | Chengdong Lake . | basin subsystem losses . | diversion/10^{6}m^{3}
. | system target value . |

1 | 0,1 | 0.76 | 0.67 | 0.56 | 0.91 | 2.90 | 0 | 0 | 0 | 0 | 0 | 0 |

2 | 0.1,0.9 | 0.76 | 0.67 | 0.56 | 0.91 | 2.90 | 0 | 0 | 0 | 0 | 0 | −0.0725 |

3 | 0.2,0.8 | 0.76 | 0.67 | 0.56 | 0.91 | 2.90 | 0 | 0 | 0 | 0 | 0 | −0.1450 |

4 | 0.3,0.7 | 0.76 | 0.67 | 0.56 | 0.91 | 2.90 | 0 | 0 | 0 | 0 | 0 | −0.2175 |

5 | 0.4,0.6 | 0.76 | 0.67 | 0.56 | 0.91 | 2.90 | 0 | 0 | 0 | 0 | 0 | −0.2900 |

6 | 0.5,0.5 | 0.76 | 0.67 | 0.56 | 0.91 | 2.90 | 0 | 0 | 0 | 0 | 0 | −0.3625 |

7 | 0.51,0.49 | 0.760 | 0.670 | 0.560 | 0.910 | 2.900 | 0 | 0 | 0 | 0 | 0 | −0.3698 |

8 | 0.52,0.48 | 0.760 | 0.670 | 0.560 | 0.910 | 2.900 | 0 | 0 | 0 | 0 | 0 | −0.3770 |

9 | 0.53,0.47 | 0.762 | 0.672 | 0.562 | 0.912 | 2.908 | 3.65 | 0 | 0 | 3.65 | 0.11 | −0.3527 |

10 | 0.54,0.46 | 0.764 | 0.674 | 0.564 | 0.914 | 2.916 | 3.81 | 0 | 0 | 3.81 | 1.78 | −0.3604 |

11 | 0.55,0.45 | 0.766 | 0.676 | 0.566 | 0.915 | 2.923 | 3.97 | 0 | 0 | 3.97 | 3.47 | −0.3680 |

12 | 0.56,0.44 | 0.768 | 0.678 | 0.567 | 0.917 | 2.930 | 4.13 | 0 | 0 | 4.13 | 5.15 | −0.3757 |

13 | 0.57,0.43 | 0.770 | 0.680 | 0.569 | 0.919 | 2.938 | 4.29 | 0 | 0 | 4.29 | 6.80 | −0.3836 |

14 | 0.58,0.42 | 0.771 | 0.682 | 0.571 | 0.921 | 2.945 | 4.45 | 0 | 0 | 4.45 | 8.42 | −0.3915 |

15 | 0.59,0.41 | 0.773 | 0.684 | 0.573 | 0.923 | 2.953 | 4.61 | 0 | 0 | 4.61 | 10.08 | −0.3997 |

16 | 0.6,0.4 | 0.77 | 0.69 | 0.58 | 0.92 | 2.96 | 4.77 | 0 | 0 | 4.77 | 11.68 | −0.4078 |

17 | 0.7,0.3 | 0.78 | 0.71 | 0.59 | 0.94 | 3.02 | 5.89 | 0 | 0 | 5.89 | 23.06 | −0.4949 |

18 | 0.8,0.2 | 0.80 | 0.72 | 0.61 | 0.95 | 3.08 | 7.02 | 0 | 0 | 7.02 | 34.83 | −0.5893 |

19 | 0.9,0.1 | 0.82 | 0.73 | 0.62 | 0.97 | 3.14 | 8.14 | 0 | 0 | 8.14 | 47.35 | −0.6910 |

20 | 1,0 | 0.84 | 0.74 | 0.63 | 0.98 | 3.19 | 9.26 | 0 | 0 | 9.26 | 62.06 | −0.7975 |

Table 4 lists large scale system joint operation results under 20 weight programs, which basically reflect the non-inferior solutions in the two contradictory subsystem problems in this large scale system. Large scale system target values are the numerical significance reflected by combining the two contradictory subsystem problems by weighting method, which vary with the weight ratio. In this study, the start water level in each reservoir is real-time status water level, the group reservoir subsystem safety ranges from 2.90 to 3.19. The small variation range indicated inflow water volume is relatively small for each reservoir, each flood storage basin has enough surplus flood storage capacity, and the joint operation can be achieved by simply opening Qiujia Lake to store excess flood. Flood storage basin subsystem loss is located between 0 and 9.26, which indicates that total diversion flood volume is not large.

Figure 4 shows that reservoir group subsystem safety increases with the increase of its own weights, which meets positive correlation. The larger reservoir group weight means the more important reservoir group subsystem safety, thus, the smaller flood control storage needed in the reservoir group, and the larger reservoir group subsystem safety. In this study, when reservoir group weight , only the reservoir group joint operation is needed to control flood and guarantee safety discharge at control section, the corresponding reservoir group subsystem safety is 2.90. When reservoir group weight , we need reservoir group and flood storage basin joint operation to guarantee safety discharge at control section due to the minimum of large scale system objective function. The reservoir group weight 0.53 is a turning point, reservoir group subsystem safety gradually increases with the increase of reservoir group weights.

Figure 5 demonstrates that flood storage basin subsystem losses decrease with the increase of its own weights, which meets negative correlation. The larger flood storage basin weight means the more important flood storage basin subsystem losses. As a result, the smaller diversion volume needed in flood storage basin, and the smaller flood storage basin subsystem losses. In this study, when flood storage basin weight , we need reservoir group and flood storage basin joint operation to guarantee safety discharge at control section, flood storage basin subsystem losses gradually decrease with the increase of flood storage basin weights. Meanwhile, flood storage basin weight 0.47 is a turning point, there is a jumping phenomenon at turning point in Figure 5, which resulted from initial water volume in flood storage basin as shown in Equation (5), that is, flood storage basin losses are determined by both initial water volume and diversion volume, and can also be corresponding to the constant of once diversion losses. When flood storage basin weight , flood control task can be done independently by reservoir group without the use of flood storage basins. Thus, flood storage basin subsystem loss is 0 at this time.

Figure 6 presents the non-inferior solutions between reservoir group subsystem safety and flood storage basin subsystem losses in this large scale system. In this study, when reservoir group weight is less than 0.53, namely flood storage basin weight is greater than 0.47, the relationship between the two subsystem problems is a point, as shown with the solid point in Figure 6; when reservoir group weight is greater than 0.53, namely flood storage basin weight is less than 0.47, the relationship between the two subsystem problems is a positive correlation, constituting the non-inferior solution space, as shown with the hollow points and dotted line in Figure 6. In real-time operation, based on the actual flood situation, expertise and other factors, decision-makers choose appropriate weight ratio under a certain decision preference for joint control flood to gain system flood control benefit. This model has a better decision adaptability than a single-objective optimization model.

Figure 7 demonstrates that the safety discharge at Lutaizi control section can be guaranteed by undertaking the excess flood process through four reservoirs to effectively reduce flood peak and Qiujia Lake to store excess flood in the condition of large scale system global optimum. Results show that the third-order hierarchical decomposition–coordination model is effective.

## CONCLUSIONS

A third-order hierarchical decomposition–coordination model for joint flood control of reservoir group and flood storage basin was proposed in this paper and the optimal calculation method and coordination method based on large scale system theory was suggested. The model was applied for real-time flood control operation in the middle reaches of Huaihe River and it has the following characteristics:

The model decomposes the complex flood control system into several subsystems in accordance with spatial distribution. It has a clear hierarchical structure and independent solution method, which can effectively reduce the large scale system dimension, to a certain extent, and avoid the ‘dimensions disaster’ problem.

The model is flexible. Large scale system theory guarantees different optimal orders and different optimal methods among different subsystems which are decomposed from complex large scale system. The specific form of model and solution method for reservoir, flood routing, and flood storage basin can be chosen flexibly, which is convenient for subsystem independent optimal calculation and similar flood control system application.

The model has some versatility and maneuverability. Considering the requirements of real-time flood control operation, the model supports decision-making of human–computer interactions and maximizes the benefits in flood control and disaster mitigation through the rolling flood control operation.

## ACKNOWLEDGEMENTS

This study has been funded by National Scientific Program for Global Change Research of China (973 Program) (Grant No. 2010CB951102), National Natural Science Foundation of China (Grant No. 51179044) and National Scientific Program for Cascade Reservoirs Risk Warning of China (973 Program) (Grant No. 2013CB036406). The help provided by Associate Professor Simin Qu and PhD Peng Jiang in modifying this paper in English is appreciated. The authors would also like to thank the editor and anonymous reviewers for their reviews and valuable comments related to this manuscript.