Severe droughts typically last for extended periods and result in substantial water shortages, posing challenges for water conservancy projects. This study proposed a framework for coordinating drought mitigation operations across projects of various scales. First, the regulation and drought mitigation capacities of each project were analyzed, and thus critical reservoirs was identified. Subsequently, a joint regulation model for water supply, prioritizing projects based on their regulatory capacity from weak to strong, was established. An optimization model is then developed to determine the drought-limited levels for critical reservoirs, aiming to minimize water shortages. This model facilitates temporal coordination of water resources to prevent severe water shortages with frequent mild water shortages. Results in the Chuxionglucheng District of Chuxiong, Yunnan Province, during the severe drought period from 2009 to 2013 demonstrate significant reductions in water shortage. Specifically, the maximum shortage ratio decreased from 59 to 45% for agriculture and from 52 to 8% for industry. Moreover, emergency measures for drought mitigation were compared and recommended for regions with weak projects regulation. Overall, this framework offers a systematic approach to enhancing drought resilience across diverse water conservancy projects in severe drought conditions.

  • Coordinating drought mitigation operations across projects of various scales is proposed.

  • Optimal drought-limited water levels are optimized for the critical reservoirs.

  • The coordinating operation and optimal hedging rules decrease the water shortage during the extreme drought.

Drought is one of the most serious climatic hazards (Borgomeo et al. 2015; Zhang et al. 2022c; Zaniolo et al. 2023). Due to the combined effects of climate change and human activities, water shortage and drought events have become more frequent and severe in recent decades (Jehanzaib et al. 2020; Zhang et al. 2022a; Wang et al. 2023b). Some regions have even suffered from record-breaking extreme droughts, which undoubtedly pose a great threat to both economic and social development and the safety of people's lives (Lopez-Nicolas et al. 2017; Ault 2020; Wang et al. 2023a).

The frequent occurrence of drought events has attracted the attention of scholars. They have carried out extensive research on drought indicators (Vicente-Serrano et al. 2010; Shah & Mishra 2020; Lin et al. 2023b), drought prediction (Fung et al. 2020; Pan et al. 2023; Pande et al. 2023), drought assessment (Karnieli et al. 2010; Veijalainen et al. 2019; Meza et al. 2020), and so on. Also for drought mitigation, scientific scheduling of water conservation projects is regarded as the most essential and effective measure (Tu et al. 2003; Wu et al. 2019; Zhang et al. 2022b). Based on the regulation capacity of the water conservation projects, the mismatch between the natural inflow and the water usage can be improved to maximally meet water demand, and mitigate the adverse impact of droughts. Research shows that the reservoir hedging rule is effective, which rations water supply slightly in the current period and reserves water for future use, thus avoiding severe water shortage events in the future (Karamouz & Araghinejad 2008; Seo et al. 2019; Luo et al. 2023). For instance, Chang et al.(2019) proposed a hedging policy triggered by the seasonal drought prevention limiting water level (DPLWL), and its use in the Yellow River Basin proved the superiority of the proposed hedging rule. Meanwhile, the improved rules perform better during normal drought events and with individual drought years than severe droughts or with successive drought years. Zhang et al. (2022b) divided the static drought-limited water level into dynamic drought warning water level and drought depletion water level. The optimal dynamic controlling scheme of a multi-year regulation reservoir effectively reduced agricultural crop yield loss risk due to drought disasters. All these drought mitigation studies demonstrate the superiority of hedging rule optimization in reducing regional water shortage.

However, these existing studies generally targeted moderate droughts (Shih & ReVelle 1995; Jin & Lee 2019; Raso et al. 2019). Its conflict between water supply and demand can be well resolved by optimizing the hedging rules of the single reservoir or simple reservoir group system (Choi et al. 2020; Lin et al. 2023a). Yet the extreme droughts of concern in this paper impact water supply over a wide range. Thus, mitigation of severe drought involves numerous water sources, users, and water conservation projects (Cunha et al. 2019; Zhang & Shen 2019). The projects include the inter-basin water transfer project, the reservoirs of different scales, and the micro conservation projects. Different projects have different regulation capacity, water users, and different resistance ability for drought, especially for severe droughts. How to rationally utilize all these water conservancy projects with different regulation capacities to satisfy the water demand of different water users is an essential issue (Chae et al. 2022; Kim et al. 2022).

To address the above issue, a joint operation framework of large, medium, small, and micro water conservation projects for drought mitigation is constructed in this study. In this framework, we firstly simplified the system complexity through the critical water source identification and cooperative regulation mode development. Subsequently, an optimization model of drought-limited water levels is established for the critical reservoirs. The hedging rules are optimized to minimize the water shortage indexes for each user, enabling the temporal reallocation of water resources. Finally, multiple emergency regulation scenarios will be formulated for regions whose water demand are still unsatisfied. Through these three steps, severe drought damages will be mitigated during mega-droughts.

The flowchart of the proposed framework for extreme drought mitigation is shown in Figure 1. It consists of three sub-models, i.e., a coordinate operation model, an optimal dispatch model, and an emergency operation model. In the first step, the water supply–demand network should be established and the effects of different projects should be evaluated. Second, the identified critical reservoirs are aggregated, and their hedging rules are optimized to fully utilize the storage capacity and mitigate drought impacts. Ultimately, for extreme droughts with unmet water demand, the emergency operation model further increases water supply or reduces water demand based on the emergency measures to alleviate the huge supply–demand contradiction. The detailed settings of each sub-model will be introduced in this section in turn.
Figure 1

The flowchart of the proposed drought mitigation framework.

Figure 1

The flowchart of the proposed drought mitigation framework.

Close modal

Cooperative regulation framework of hydraulic engineering projects

Extreme droughts are characterized by prolonged durations and high intensities, and it is necessary to coordinated operate all the water conservation projects together to effectively mitigate the drought damages. Typically, these projects include underground and groundwater projects, such as the regional water diversion projects, and inter-basin water transfer projects. Among these, the regional and inter-basin water transfer projects can reallocate the water resources in spatial, and reservoirs can reallocate the water resources in temporal. The various sizes of reservoirs serve different functions in drought mitigation, as outlined in the following,

  • (1) Large and medium-sized reservoirs have strong storage regulation ability and are the backbone reservoirs against mega-droughts. These reservoirs can reserve water during wet years, creating a reserve for use during drought years, thereby playing a critical role in prolonged drought mitigation. Additionally, in the face of intense drought, reservoirs with high capacity have a surplus of available water for supply, while low-capacity reservoirs may face empty storage. In essence, reservoirs with higher regulation capacities exhibit superior drought resistance capabilities, and the optimal operation of these reservoirs is vital for drought mitigation.

  • (2) Small-sized reservoirs have weak storage regulation ability and usually experience the situation of empty and thus no water to be supplied during the droughts. Nevertheless, they can supply more water in the early stage of drought to reduce the water supply pressure on large-size reservoirs and thus increase their water supply capacity during the mega-drought events.

  • (3) The micro-projects, such as the water delivery trucks and underground pumping wells, are very flexible. Their agility in responding to localized water shortages contributes significantly to ensuring water security during drought events.

Therefore, this study proposes a framework for the joint operation of large, medium, small, and micro water conservation projects to optimize their respective roles in the drought mitigation. This framework consists of three sub-models, outlined as follows.

First, establish the supply–demand relationship between the water source projects and the water consumers by creating a supply–demand network diagram. On the demand side, determine the regular water demand and the minimum water demand during droughts, along with the priority of different water consumers. On the water supply side, analyze the water supply capacity of various projects and determine their maximum water supply capacity during droughts.

Second, establish a cooperative regulation mode for various hydraulic engineering projects. In this mode, the projects supply water in order of their regulation capacities, from weak to strong. Specifically, water from the inter-basin water diversion project supplies first, followed by the small, medium, and large-scale reservoirs. Additionally, optimize the operation rules, known as the hedging rules, of the critical reservoirs, particularly the large-scale reservoir. Hedging rules, triggered by drought-limited water levels (DLWL), are optimized to allocate water resources in temporal, thereby avoiding extreme water shortages instead of frequent minor shortages.

Third, during the severe drought events, the water demand may not be satisfied in the regions with weak regulation capacity projects. Therefore, an emergency regulation module should be activated to implement emergency water supply measures when significant water shortages persist. These emergency measures include reducing or suspending water demand from users, such as suspending industrial water consumption. Additionally, enhancing decentralized water supply infrastructure, such as the pumping wells and water tankers, should be considered.

The second mode is the critical part of the framework, and thus following sections introduce the optimization of the hedging rules of critical reservoirs.

The aggregation–decomposition model

There might be multiple critical reservoirs in the study region, i.e., a multi-reservoir system, and the aggregation–decomposition method is adopted to aggregate the multiple reservoirs to a virtual reservoir.

  • (1) The aggregate model

The storage of the aggregate reservoir is the cumulative storage of all individual reservoirs.
(1)
where denotes the ending storage of the aggregate reservoir at time t, and is the ending storage of reservoir i at time t, and N is the number of reservoirs.
The inflow of the aggregate reservoir is the natural inflow of the multi-reservoir system, excluding the release from the upstream reservoirs flowing into the downstream reservoir.
(2)
where denotes the natural inflow of reservoir i at time t.
There are often four types of water users, agriculture, industrial, domestic, and ecological users, and the water demand of the aggregate reservoir is the total of all water users of the multi-reservoir system.
(3)
(4)
(5)
(6)
where , , , and represent the water demand of ecology, industry, domestic, and agriculture of the aggregate reservoir at time t. , , , and represent the water supply from reservoir i to region k at time t. M is the number of water use regions when the reservoir supplies to multiple regions.
  • (2) Decomposition model

The release of the aggregate reservoir is the total release of the multi-reservoir system, and it should be distributed to each individual reservoir. The distribution or partition scheme significantly affects reservoir storage compensation and water resource utilization efficiency. This study allocates the joint water supply into each reservoir based on a partition ratio. This ratio is defined as the portion of water availability of reservoir i compared to the total water availability of all reservoirs with a common demand, as shown in the following.
(7)
where is the water supplied by reservoir i.

According to Equation (7), the partition ratio varies over time, and the reservoir with greater water availability supplies more water. This suggests effective utilization of reservoir capacity compensation. However, the reservoir regulation capacity is not considered in the partition ratio, and this might lead to water spillage for the reservoirs with weak regulation capacity. Therefore, Equation (7) is applied to determine the initial value of the partial ratio, and it will be enlarged for the reservoir with spillage, ensuring water utilization efficiency.

Multi-reservoir hedging rules optimization

Hedging rules

Hedging rules are widely used for drought mitigation. It avoids a severe water shortage in the future through slight water shortages in the current period. Previous studies have demonstrated the effectiveness of hedging rules in alleviating droughts. The triggers of the hedging rule include reservoir water levels (Tu et al. 2003; Chang et al. 2005), available water (You & Cai 2008; Shiau 2011), and so on (Giuliani et al. 2015; Denaro et al. 2017). In this study, reservoir water levels are employed as triggers, defined as drought-limited water levels (DLWL). There are two levels, defined by drought warned water level (DWWL) and drought protected water level (DPWL), as defined by Luo et al. (2023), and depicted in Figure 2. Also, the amount of water supplied by the reservoir can be expressed as the following equation,
(8)
where is the total amount of water supplied by the aggregate reservoir. , , , are optimal water supply for ecology, agriculture, industry, and domestic, respectively. , , , are the restriction ratios for the corresponding water users, and they take different values when the water level falls in different sub-zones of Figure 2.
Figure 2

Schematic of reservoir drought-limited water levels.

Figure 2

Schematic of reservoir drought-limited water levels.

Close modal

When the reservoir water level is higher than the DWWL, the water demand of all water users can be met. When the water level falls below the DWWL but remains above the DPWL, the water supply needs of higher-priority users can be satisfied, while those with lower priority are restricted. When the water level drops below the DPWL, the water supply requirement of all water users should be restricted. These restriction ratios can be optimized, typically set at 0.7 for agriculture and 0.9 for domestic and industrial water supply.

In order to optimize the DLWLs, an optimization model should be established, introduced as follows.

Optimization model

  • (1) Objectives

There are typically four types of water users: agriculture, industrial, domestic, and ecological users, and they compete with each other, especially during droughts. Among them, ecological users have the highest water supply priority which is determined by the concept of green development in this region. It is then followed by domestic and industrial users, with agriculture having the lowest priority. Different water supply strategies result in varying drought mitigation effects, including the frequency, severity, and duration of water scarcity. This study adopts a comprehensive indicator, the water shortage index, proposed by the U.S. Army Corps of Engineers (1971), to assess the water shortage risk for each user. This indicator effectively reflects the overall water scarcity risk, encompassing frequency, severity, and duration. Moreover, greater water scarcity leads to larger economic losses, which should be avoided. Therefore, the quadratic of water shortage index is adopted. The objectives of the optimization model are described as follows.

Minimization of water shortage index for ecology,
(9)
Minimization of water shortage index for agriculture,
(10)
Minimization of water shortage index for industry,
(11)
Minimization of water shortage index for domestic,
(12)
X represents the set of variables, which are the drought-limited water levels as shown in Figure 2.
  • (2) Constraints

    • (a) Mass balance equation of the aggregate reservoir
      (13)
      where , are the storage for reservoir i at time t and t+ 1, , , are total water supply, evaporation and leak loss, and spillage of the aggregate reservoir at time t, respectively.
    • (b) Water level limits
      (14)
      where is the active water level in non-flood season and the flood limited water level in flood season.
    • (c) The hydraulic connections between reservoirs

For the cascaded reservoir system, the inflow of the downstream reservoir comes from the release from the upstream reservoir and the flow from the interval region. The release from upstream to downstream includes the spillage and the ecological water supply, shown as follows,
(15)
  • (d) The water supply is not higher than the demand,
    (16)
    where j denotes the jth water user (including ecology, industry, agriculture, and domestic), and Wj,t is the water supply of jth user from all the reservoirs
  • (e) The reliability of all water users should satisfy the designed requirement (denoted by Pj,d)
    (17)
  • (f) The shortage ratio of all water users should also be not higher than the designed value (denoted by ), as shown in the following equation
    (18)
  • (3) Algorithm to solve the model

The effectiveness of ε-NSGAII in solving multiobjective optimization problems has been demonstrated in various studies (Kasprzyk et al. 2012, 2013, 2017). Regarded as a top-performing search tool among the state-of-the-art multiobjective evolutionary algorithms (Reed et al. 2013), ε-NSGAII ensures both convergence and diversity of the Pareto approximate set by employing an ε-dominance archive and adaptive population sizing. Hence, it is adopted to optimize DLWL. For details regarding parameter settings of this algorithm, please refer to previous research (Zhang et al. 2017). To eliminate the effect of population generation uncertainty, we conduct 10 random-seed runs. Each run employs ε-NSGAII for 500,000 evaluations. The final Pareto approximate set is obtained by combining the best individuals across all runs with a nondominated sort.

Yunnan Province, located in southwestern China (as shown in Figure 3), is a high-risk area for drought, experiencing a moderate drought approximately every three years and a slight drought every two years. Since 2000, the runoff in Yunnan Province has been lower than the annual average. Notably, it experienced a historical anomaly, unprecedented and prolonged drought from 2009 to 2013. As illustrated in Figure 4, the annual runoff during the period is below that of the frequency of 75% and even as low as 95%. Therefore, it is urgent to develop a scientific and practical drought mitigation scheme for this region.
Figure 3

Location of Chuxiong.

Figure 3

Location of Chuxiong.

Close modal
Figure 4

Runoff in Jiulongdian and Qingshanzui Reservoir (a, b), water demand process and ratio for different water users in the Chuxionglucheng District (c, d).

Figure 4

Runoff in Jiulongdian and Qingshanzui Reservoir (a, b), water demand process and ratio for different water users in the Chuxionglucheng District (c, d).

Close modal

The water scarcity situation is particularly severe in Chuxiong Prefecture, located in the central part of Yunnan Province, covering a total area of 28,438 km². The climate in this region is subtropical monsoon, with the flood season lasting from May to October, and the dry season lasting from November to April. The Chuxionglucheng District, serving as the primary water receiving district in Chuxiong, is taken a case study. The water resources project group in Chuxiong Prefecture includes one large-scale reservoir (QingShanZui Reservoir), three medium-scale reservoirs (Jiulongdian, Zhongshiba, and Xijinghe Reservoirs), over 100 small-scale reservoirs, and the Central Yunnan Water Transfer Project. The projected annual water demand in Chuxionglucheng for the year 2,040 is 319.52 million m3, with industrial and agricultural sectors constituting 69% of this demand. The water demand process is depicted in Figure 4(c) and 4(d).

For comparison, a region with weak regulation hydraulic engineering projects, Nanhualongchuan District, is selected to validate the performance of the proposed framework. The water engineering projects include inter-basin diversion, Laochanghe Reservoir, Maobanqiao Reservoir, and Xijinghe mid-size reservoirs, along with small-scale reservoirs and local water diversion and lifting projects. The total active reservoir storage of three medium reservoirs is 30.91 million m3. The water demand is 71.93 million m3.

Coordinated operation of the hydraulic engineering projects

As demonstrated in Section 3, there are numerous hydraulic projects in the Chuxionglucheng District. Coordinating the regulation of the water conservancy projects to optimize their regulatory functions and efficiently utilize water resources poses a significant challenge. To address this challenge, we firstly evaluate the regulatory capacity of each project, measured by the ratio between the active storage and average annual runoff. Table 1 illustrates that Qingshanzui Reservoir is the key water source during droughts in Chuxionglucheng, since it is an over-year and large-size reservoir.

Table 1

The drought mitigation of different reservoirs in the Chuxionglucheng District

JiulongdianXijingheZhongshibaQingshanzui
Size of the reservoir Mid-size Mid-size Mid-size Large-size 
Regulation capacity Over-year Over-year yearly Over-year 
Active storage (104 m35,912 898 632 6,202 
Water demand (104 m33,285 1,195 424 8,121 
Water supply (104 m32009 3,285 819 424 8,121 
2010 3,285 251 424 8,121 
2011 3,285 46 424 7,252 
2012 2,917 33 233 5,327 
2013 3,285 148 180 8,121 
Drought resistance index 2009 1.00 0.69 1.00 1.00 
2010 1.00 0.21 1.00 1.00 
2011 1.00 0.04 1.00 0.89 
2012 0.89 0.03 0.55 0.66 
2013 1.00 0.12 0.42 1.00 
JiulongdianXijingheZhongshibaQingshanzui
Size of the reservoir Mid-size Mid-size Mid-size Large-size 
Regulation capacity Over-year Over-year yearly Over-year 
Active storage (104 m35,912 898 632 6,202 
Water demand (104 m33,285 1,195 424 8,121 
Water supply (104 m32009 3,285 819 424 8,121 
2010 3,285 251 424 8,121 
2011 3,285 46 424 7,252 
2012 2,917 33 233 5,327 
2013 3,285 148 180 8,121 
Drought resistance index 2009 1.00 0.69 1.00 1.00 
2010 1.00 0.21 1.00 1.00 
2011 1.00 0.04 1.00 0.89 
2012 0.89 0.03 0.55 0.66 
2013 1.00 0.12 0.42 1.00 

Second, the significance of a reservoir is greater when it has a larger water supply volume and supplies users with higher priority. In the Chuxionglucheng District, Qingshanzui and Jiulongdian reservoirs play a crucial role, as they supply 90% of the region's water demand to users with high priority. Specifically, Jiulongdian Reservoir supplies domestic users, while QingShanZui Reservoir mainly serves industrial users.

Third, the water storage projects play a higher role when they have higher drought mitigation capacity. This study employs a drought resistance index defined by the ratio of reservoir's available water supply to the total required water supply, with the results listed in Table 1. Additionally, Figure 5 shows the variation of the storage of the small-size reservoirs, which are aggregated as one virtual reservoir. Results indicate that Jiulongdian Reservoir exhibits the highest drought resistance, followed by QingShanZui Reservoir and Zhongshiba Reservoir. Conversely, small-size and medium-size reservoirs have little or no available water during droughts.
Figure 5

The variation of reservoir storage for small-scale reservoirs. (a) Starting water storages by year from 1961 to 2020 and (b) starting water storages by month from 2009 to 2013.

Figure 5

The variation of reservoir storage for small-scale reservoirs. (a) Starting water storages by year from 1961 to 2020 and (b) starting water storages by month from 2009 to 2013.

Close modal

Considering the above three factors, it is concluded that QingShanZui and Jiulongdian Reservoirs are the critical water sources for drought mitigation in the Chuxionglucheng District.

Furthermore, in conjunction with the regulatory performance of each reservoir, the prioritized sequence principle for the use of water sources ranges from weak to strong regulatory capabilities. Subsequently, a coordinated control scheme for the hydraulic engineering group in the study area was established: for domestic and industrial water supply, the preferred order of water resources is Dianzhong Diversion Water, followed by small-scale reservoirs, and then medium-sized and large-scale reservoirs. For agricultural irrigation use, priority is given to water diversion from the river, small-scale reservoirs, and Dianzhong Diversion Water, with medium and large-scale reservoirs as the next option.

Hedging rules for Qingshanzui-Jiulongdian cascaded reservoirs

According to the coordinated operation principle proposed in the last section, which prioritizes utilizing water resources from low-capacity reservoirs, the remaining water demand from the entire Chuxionglucheng region should be met by the Qingshanzui Reservoir and Jiulongdian Reservoir. The water supply from the two reservoirs should meet the following criteria to ensure the water security of Chuxionglucheng.

  • (1) Water shortage ratio

    • a. Agricultural water supply: The shortage ratio should not exceed 0.54.

    • b. Industrial and domestic water supply: The shortage ratio should not exceed 0.11.

  • (2) Reliability

    • a. Agricultural water supply: The reliability should not be less than 0.75.

    • b. Industrial and domestic water supply: The reliability should not be less than 0.95.

Given that the reliabilities of domestic and industry water use are both set as 95%, these two users are merged into a single user, referred to the public water user. Figure 6 illustrates the Pareto approximate sets of the aggregated reservoir, with water supply tasks illustrated in Figure 4. The ecological water use during the main flood season is set at 30% of the multi-year average natural runoff and reduced to 10% during the non-main flood season.
Figure 6

Pareto approximate sets of the aggregated reservoir.

Figure 6

Pareto approximate sets of the aggregated reservoir.

Close modal

In the figure, the arrow directions indicate the preferred objectives, with the ideal optimal solution located at the left corner of the graph. It is observed that there exists a non-linear competitive relationship between the shortage indexes of public and agriculture. That is to say, improving the water supply benefits for public water uses will inevitably reduce that for agriculture.

A satisfied solution, with the smallest Euclidean distance to the ideal optimal solution, is marked with a rectangular box in Figure 6. This solution is selected for detailed analysis in the subsequent section, along with the corresponding optimal DLWLs shown in Figure 7. As illustrated in Figure 7(a), the DWWL locates above the DPWL with the peak value in May, the peak period of irrigation. The reason for this is that elevating the DWLW will induce a higher frequency of water supply restriction, resulting in more water stored in the reservoir. This stored water can be utilized during the periods of water shortage. When the restricted water supply ratio is the same across different periods, restricting water supply during high-demand periods leads to greater water retention, thereby significantly reducing the shortage ratio and frequency compared to restricting supply during low-demand periods. This finding has also been verified in existing studies (Luo et al. 2023).
Figure 7

Optimal hedging rules of the aggregated reservoir of Qingshanzui and Jiulongdian (a), and partition ratios of water supply for the common water demand (b).

Figure 7

Optimal hedging rules of the aggregated reservoir of Qingshanzui and Jiulongdian (a), and partition ratios of water supply for the common water demand (b).

Close modal

Figure 7(b) illustrates the average partition coefficients of water supply for different years. As illustrated in the figure, on the whole, the water supply partition ratio of Qingshanzui Reservoir is more than three times that of Jiulongdian Reservoir. This can be attributed to the fact that the Qingshanzui Reservoir is a large-scale reservoir with strong storage capacity and much water to be supplied. Furthermore, the water supply partition ratio of Qingshanzui Reservoir is notably high during the flood season. This is because Qingshanzui Reservoir locates in the mainstream of the Longchuan River, where water availability is abundant during this period.

Drought mitigation effects during severe drought

For comparison, a conventional scenario, which also follows the coordinated operation principle but applies a standard operating procedure (SOP) for all reservoirs, is considered. The optimal scenario uses the coordinated operation principle and the optimal hedging rule of the critical reservoirs, i.e., the rule shown in Figure 7. These two scenarios are taken to simulate the reservoir operation during the consecutive extreme drought from 2009 to 2013, with results presented in Figure 8. Compared with the conventional scenario, the maximum water shortage ratio decreased significantly from 59 to 45% for agriculture, and from 52 to 8% for industry. However, there has been an increase in the number of periods with water shortages. That is, the optimal reservoir operation strategy leads to frequent small-scale water shortages, thereby mitigating the occurrence and severity of extreme water shortage events.
Figure 8

The water shortages under two scenarios in the Chuxionglucheng District during the period 2009–2013.

Figure 8

The water shortages under two scenarios in the Chuxionglucheng District during the period 2009–2013.

Close modal

The results indicate that the integrated operation of all conservation engineering projects and the optimal drought mitigation scheme can effectively alleviate the adverse impact of drought.

Emergency regulation scenario in weak regulation region

This section validates the performance of the engineering projects in the region when there is an absence of large-scale water storage projects. The prolonged drought period from 2009 to 2013 is taken as the case study and the results are shown in Figure 9. As demonstrated by the solid curves, even with the synergistic regulation of multiple water sources and optimization of critical water resources, there still exists a severe water shortage issue. The domestic and agriculture shortage ratios are 71 and 74%, respectively. These water shortage ratios have exceeded the sustainable threshold required to guarantee the safety of water usage in both industrial and agricultural sectors due to the weak regulation of reservoirs. Emergency water supply measures are urgently needed to mitigate droughts and water shortages.
Figure 9

The water shortages for different water users in the Nanhualongchuan District during the period of 2009–2013.

Figure 9

The water shortages for different water users in the Nanhualongchuan District during the period of 2009–2013.

Close modal

As can be seen from the optimal scenario, since July 2011, there has been little water in the reservoir, resulting in no water available for industrial use. This indicates a severe water shortage event. Therefore, to prevent a concentrated and severe drought, the water resources should be evenly distributed over time, meaning that the water demand should be restricted when a light drought occurs. Meanwhile, there are high shortages in both domestic and industrial sectors, which both rely on Laochanghe Reservoir. Therefore, a scenario for adjusting the water supply structure is proposed, shown as scenario 2. Finally, during a drought, ecological water demand can also be restricted to reserve water for domestic and industrial use, which is scenario 3. The details of the three emergency scenarios are as follows.

Emergency scenario 1: Restricting water demand. The industrial water demand is restricted to 90%, and agriculture water supply is restricted to 50% in Laochanghe Reservoir.

Emergency scenario 2: Adjusting the water supply structure. Laochanghe Reservoir no longer supplies agricultural water use, and restricts the industry to 90% after satisfying the water demand of domestic.

Emergency scenario 3: based on scenario 2, restrict the ecological flow to 10% of the multi-year average streamflow.

As depicted in Figure 9, the periods of water scarcity for industrial and domestic use are postponed, and the duration of water scarcity is significantly reduced. Comparing the dotted curves (Scenario 1) and the solid curves, it is evident that the water shortages in 2011 is improved, but they are not alleviated in 2012–2013. When suspending the agricultural water supply in the Laochanghe Reservoir (Scenario 2), the periods of water shortages for domestic and industry can be further decreased. The occurrences of water shortage for domestic and industrial users are reduced from 27 and 19 times to 25 and 18 times, respectively. Nevertheless, the maximum shortage ratios for industry and agriculture are still the same as the original scenario. This can be improved by imposing restrictions on ecological supply. In scenario 3, the maximum water shortage is reduced to 53%, occurring only once. These results indicate that, by curtailing ecological and agricultural water use, it is possible to significantly mitigate both the severity and duration of water scarcity for domestic and industrial, thereby ameliorating the adverse impacts of drought.

However, the water shortage ratio for domestic 53% is still high. To guarantee the basic water demand, it is necessary to initiate unconventional emergency water sources. This can be achieved by increasing groundwater extraction, augmenting the water diversion volume, and implementing mobile water delivery vehicles to remote regions. Simultaneously, consider the appropriate utilization of the reservoir storage below the dead storage capacity, and so on to prevent severe water shortages.

Severe droughts are occurring more frequently under changing environment. Severe droughts require the coordination of all water engineering projects to mitigate the adverse effects of drought. To this end, this study proposes a framework for the joint operation of multiple water conservation projects tailored heavy and extreme drought. The framework comprises three sub-models: a coordinate operation model for the water conservation projects, an optimal dispatch model for drought mitigation of the critical reservoirs, and an emergency operation model for extreme droughts. The results of the case study conducted in Chuxiong Prefecture indicate that the proposed framework effectively alleviates the water shortages during heavy drought and extreme drought. Specifically, the maximum water shortage ratio decreased from 59 to 45% for agriculture users and from 52 to 8% for industry users.

The proposed drought operation framework provides a novel water supply strategy to fully utilize limited water resources. However, it is developed only based on historical drought processes, and incorporating real-time monitoring and forecasting information is further needed for better optimization of water resources allocation. In addition, the proposed framework only restricted water supply to users in emergency scenarios of the study area, while it can be applied to more drought-stricken areas in future studies, and increase more water supply by activating emergency water sources, such as appropriately utilizing the dead storage capacity.

This research is supported by the National Key Research and Development Program of China (No. 2021YFC3000205) and the Open Research Fund of Hubei Provincial Key Laboratory of Intelligent Yangtze River and Hydropower Science (ZH2102000102).

Data cannot be made publicly available; readers should contact the corresponding author for details.

The authors declare there is no conflict.

Ault
T. R.
2020
On the essentials of drought in a changing climate
.
Science
368
(
6488SI
),
256
260
.
Chae
H.
,
Ji
J.
,
Lee
E.
,
Lee
S.
,
Choi
Y.
,
Yi
S.
&
Yi
J.
2022
Assessment of activating reservoir emergency storage in climate-change-fueled extreme drought
.
Water
14
(
20
),
3242
.
Chang
F. J.
,
Chen
L.
&
Chang
L. C.
2005
Optimizing the reservoir operating rule curves by genetic algorithms
.
Hydrological Processes
19
(
11
),
2277
2289
.
Chang
J.
,
Guo
A.
,
Wang
Y.
,
Ha
Y.
,
Zhang
R.
,
Xue
L.
&
Tu
Z.
2019
Reservoir operations to mitigate drought effects with a hedging policy triggered by the drought prevention limiting water level
.
Water Resources Research
55
(
2
),
904
922
.
Choi
Y.
,
Lee
E.
,
Ji
J.
,
Ahn
J.
,
Kim
T.
&
Yi
J.
2020
Development and evaluation of the hydropower reservoir rule curve for a sustainable water supply
.
Sustainability
12
(
22
),
9641
.
Cunha
A. P. M. A.
,
Zeri
M.
,
Leal
K. D.
,
Costa
L.
,
Cuartas
L. A.
,
Marengo
J. A.
,
Tomasella
J.
,
Vieira
R. M.
,
Barbosa
A. A.
,
Cunningham
C.
,
Cal Garcia
J. V.
,
Broedel
E.
,
Alvala
R.
&
Ribeiro-Neto
G.
2019
Extreme drought events over Brazil from 2011 to 2019
.
Atmosphere
10
,
64211
.
Denaro
S.
,
Anghileri
D.
,
Giuliani
M.
&
Castelletti
A.
2017
Informing the operations of water reservoirs over multiple temporal scales by direct use of hydro-meteorological data
.
Advances in Water Resources
103
,
51
63
.
Fung
K. F.
,
Huang
Y. F.
,
Koo
C. H.
&
Soh
Y. W.
2020
Drought forecasting: A review of modelling approaches 2007–2017
.
Journal of Water and Climate Change
11
(
3
),
771
799
.
Giuliani
M.
,
Pianosi
F.
&
Castelletti
A.
2015
Making the most of data: An information selection and assessment framework to improve water systems operations
.
Water Resources Research
51
(
11
),
9073
9093
.
Hydrologic, E.C.U
1971
Hydrologic Engineering Methods for Water Resources Development: Principles of Ground-Water Hydrology
, Vol.
10
.
Hydrologic Engineering Center, Corps of Engineers, US Army
,
Davis, CA
.
Jehanzaib
M.
,
Sattar
M. N.
,
Lee
J.
&
Kim
T.
2020
Investigating effect of climate change on drought propagation from meteorological to hydrological drought using multi-model ensemble projections
.
Stochastic Environmental Research And Risk Assessment
34
(
1
),
7
21
.
Karamouz
M.
&
Araghinejad
S.
2008
Drought mitigation through long-term operation of reservoirs: Case study
.
Journal of Irrigation and Drainage Engineering
134
(
4
),
471
478
.
Karnieli
A.
,
Agam
N.
,
Pinker
R. T.
,
Anderson
M.
,
Imhoff
M. L.
,
Gutman
G. G.
,
Panov
N.
&
Goldberg
A.
2010
Use of NDVI and land surface temperature for drought assessment: Merits and limitations
.
Journal of Climate
23
(
3
),
618
633
.
Kasprzyk
J. R.
,
Reed
P. M.
,
Characklis
G. W.
&
Kirsch
B. R.
2012
Many-objective de Novo water supply portfolio planning under deep uncertainty
.
Environmental Modelling & Software
34
(
SI
),
87
104
.
Kasprzyk
J. R.
,
Nataraj
S.
,
Reed
P. M.
&
Lempert
R. J.
2013
Many objective robust decision making for complex environmental systems undergoing change
.
Environmental Modelling & Software
42
,
55
71
.
Kim
G. J.
,
Seo
S. B.
&
Kim
Y.
2022
Adaptive reservoir management by reforming the zone-based hedging rules against multi-year droughts
.
Water Resources Management
36
(
10
),
3575
3590
.
Lin
F.
,
Zhou
Y.
,
Ning
Z.
,
Xiong
L.
&
Chen
H.
2023a
Exploring a novel reservoir drawdown operation framework for boosting synergies of hydropower generation and drought defense
.
Sustainable Energy Technologies and Assessments
60
,
103562
.
Lopez-Nicolas
A.
,
Pulido-Velazquez
M.
&
Macian-Sorribes
H.
2017
Economic risk assessment of drought impacts on irrigated agriculture
.
Journal of Hydrology
550
,
580
589
.
Meza
I.
,
Siebert
S.
,
Doell
P.
,
Kusche
J.
,
Herbert
C.
,
Rezaei
E. E.
,
Nouri
H.
,
Gerdener
H.
,
Popat
E.
,
Frischen
J.
,
Naumann
G.
,
Vogt
J. V.
,
Walz
Y.
,
Sebesvari
Z.
&
Hagenlocher
M.
2020
Global-scale drought risk assessment for agricultural systems
.
Natural Hazards And Earth System Sciences
20
(
2
),
695
712
.
Pan
Y.
,
Zhu
Y.
,
Lue
H.
,
Yagci
A. L.
,
Fu
X.
,
Liu
E.
,
Xu
H.
,
Ding
Z.
&
Liu
R.
2023
Accuracy of agricultural drought indices and analysis of agricultural drought characteristics in China between 2000 and 2019
.
Agricultural Water Management
283
,
108305
.
Pande
C. B.
,
Kushwaha
N. L.
,
Orimoloye
I. R.
,
Kumar
R.
,
Abdo
H. G.
,
Tolche
A. D.
&
Elbeltagi
A.
2023
Comparative assessment of improved SVM method under different kernel functions for predicting multi-scale drought index
.
Water Resources Management
37
(
3
),
1367
1399
.
Reed
P. M.
,
Hadka
D.
,
Herman
J. D.
,
Kasprzyk
J. R.
&
Kollat
J. B.
2013
Evolutionary multiobjective optimization in water resources: The past, present, and future
.
Advances in Water Resources
51
,
438
456
.
Shah
D.
&
Mishra
V.
2020
Integrated drought index (IDI) for drought Monitoring and Assessment in India
.
Water Resources Research
56
,
e2019WR0262842
.
Shih
J. S.
&
ReVelle
C.
1995
Water supply operations during drought: A discrete hedging rule
.
European Journal of Operational Research
82
(
1
),
163
175
.
Tu
M. Y.
,
Hsu
N. S.
&
Yeh
W.
2003
Optimization of reservoir management and operation with hedging rules
.
Journal of Water Resources Planning And Management
129
(
2
),
86
97
.
Veijalainen, N., Ahopelto, L., Marttunen, M., Jaaskelainen, J., Britschgi, R., Orvomaa, M., Belinskij, A. & Keskinen, M.
2019
Severe drought in Finland: Modeling effects on water resources and assessing climate change impacts
.
Sustainability
11
,
24508
.
Vicente-Serrano
S. M.
,
Begueria
S.
&
Lopez-Moreno
J. I.
2010
A multiscalar drought index sensitive to global warming: The standardized precipitation evapotranspiration index
.
Journal of Climate
23
(
7
),
1696
1718
.
Wang, G., Zhang, Q., Pokhrel, Y., Farinotti, D., Wang, J., Singh, V. P. & Xu, C.
2023a
Exogenous moisture deficit fuels drought risks across China
.
npj Climate and Atmospheric Science
6
(
1
),
217
.
Wang, Y., Peng, T., He, Y., Singh, V. P., Lin, Q., Dong, X., Fan, T., Liu, J., Guo, J. & Wang, G.
2023b
Attribution analysis of non-stationary hydrological drought using the GAMLSS framework and an improved SWAT model
.
Journal of Hydrology
627
,
130420B
.
Wu
J.
,
Li
F.
,
Zhao
Y.
&
Cao
R.
2019
Determination of drought limit water level of importing reservoir in inter-basin water transfer project under changing environment
.
Theoretical and Applied Climatology
137
(
1–2
),
1529
1539
.
You
J.
&
Cai
X.
2008
Hedging rule for reservoir operations: 1. A theoretical analysis
.
Water Resources Research
44
,
W014151
.
Zaniolo
M.
,
Fletcher
S.
&
Mauter
M. S.
2023
Multi-scale planning model for robust urban drought response
.
Environmental Research Letters
18
,
0540145
.
Zhang
J.
&
Shen
Y.
2019
Spatio-temporal variations in extreme drought in China during 1961–2015
.
Journal of Geographical Sciences
29
(
1
),
67
83
.
Zhang
C.
,
Xu
B.
,
Li
Y.
&
Fu
G.
2017
Exploring the relationships among reliability, resilience, and vulnerability of water supply using many-objective analysis
.
Journal of Water Resources Planning And Management
143
(
8
),
04017044
.
Zhang, L., Kang, C., Wu, C., Yu, H., Jin, J., Zhou, Y. & Zhou, T.
2022b
Optimization of drought limited water level and operation benefit analysis of large reservoir
.
Water Resources Management
36
(
12
),
4677
4696
.
Zhang, X., Hao, Z., Singh, V. P., Zhang, Y., Feng, S., Xu, Y. & Hao, F.
2022c
Drought propagation under global warming: Characteristics, approaches, processes, and controlling factors
.
Science of the Total Environment
838
,
1560212
.
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