DRAFT for presentation at the AERE Conference, Seattle, June 2011 Collective Action and the Commons: Are Cooperative Groundwater Institutions Stable in the Presence of Environmental Externalities Encarna Esteban Gracia and Ariel Dinar Water Science and Policy Center University of California, Riverside Abstract This paper focuses on economic impacts of cooperation between groundwater users on aquifers management. Groundwater is a common pool resource with several negative externalities associated with its use. Cooperation among users is promoted as a means of achieving better management, internalizes the damages of user’s activity and reduced extractions. This paper develops a game theory framework to assess the value of cooperation in an aquifer that is being over-exploited. The framework is applied to an aquifer that is divided into three different sub-regions or sub-aquifers with different characteristics. The water extractions in each sub-aquifer affect the groundwater extractions in the other regions (extraction externality) and also the environment (environmental externality). The model is tested numerically in one of the most important aquifer in Spain, Eastern La Mancha aquifer. The results illustrate how extraction externalities and environmental externalities interact in affecting the likelihood of cooperation among the users. Keywords: cooperation, non-cooperation, externalities, common-pool resources, groundwater management, ecosystem, Shapley Value, Core, Game Theory, public choice. 1. Introduction The literature advocates public choice approaches for addressing common pool resource (CPR) problems and their optimal management. CPRs are characterized by open-access with associated congestion problems. Users of CPR can access the resource and use all the quantity they want, but the problem arises when the resource reaches a critical level of overexploitation, which triggers congestion in the use of the resource. In the case of CPRs the economic theory points out how markets by themselves are not efficient instruments to manage the resource, and public intervention is required in terms of property rights, quotas, taxes (Gordon 1954; Coase 1960; Ostrom 1990, 2010) In recent decades, several approaches have been developed to analyze different solutions to correct congestion/overexploitation of CPRs. The possible interventions can be organized into three groups: the creation of property rights (Coase 1960); the implementation of taxes and penalizations to incentive users to reduce their consumption (Pigou 1920); and finally, the creation of institutions and arrangements to incentivize users to internalize the congestion externality and cooperate for preserving these resources (Gordon 1954; Ostrom 1990, 2010). There are also studies that apply game theory approaches to check the feasibility of cooperation in CPRs and the way to achieve it (Negri 1989, Polansky et al. 2006, Dufournaud and Harrington 1990, Tarui et al. 2008, Rubio and Casino 2001, Provencher and Burt 1993, Madani and Dinar 2011). Groundwater is an example of common pool resource1. Groundwater resources are renewable resources that are used mainly for irrigation, with ‘geographically open-access’2. When there is no regulation users do not internalize the external cost, leading to pumping rates that exceed recharge and lead to congestion/overexploitation of the resource and related pollution issues (Anderson et al. 1985, Tsur 1990, 1995, Dinar 1994, Dinar and Xepapadeas 1998, Roseta-Palma 2002, Yadav 1997). While the literature provides options to deal with congestion externalities, it does not address externalities that affect stability of the CPR management 1Gordon studied the problem of CPRs in the case of fisheries harvesting. Milliman (1956) identifies that similar inefficiencies are observed in the case of groundwater. 2 For only those who have physical access to the aquifer, which is different from the case of fisheries, where everyone with access to a vessel can exploit. 2 arrangements in the presence of ecosystem damages that are different from congestion externalities. Ecosystem externalities exist when the CPR is connected to an ecosystem that can either be affected by the level of the CPR or affect the quality of the CPR, and in addition may inflict indirectly on the welfare of all users of the CPR and the society which they are part of. In this paper we introduce a cooperative game theory framework for governing groundwater resources when ecosystems are linked to the aquifers and ecosystem damages are accounted for. We hypothesize that the stability of the cooperative arrangements with and without the existence of externality cost in the form of ecosystem damages differ due to differences in the overall societal welfare. This calls for more aggressive public interventions in the case of ecosystem damages from CPR congestion. We develop a groundwater model to analyze the different users’ propensity to cooperate and the efficiency of collective action in achieving a sustainable groundwater management. We included an ecosystem health function that connects the level of water in the aquifer and the value of the linked ecosystem. The basis for cooperation in the case of existing ecosystem externalities is smaller due to lesser incremental gains to the grand coalition. The higher the ecosystem externality damage, the less the cooperative settlement will be stable. In such case, we may expect more partial coalitions (partition game) and especially when the aquifer is large and there exist many users. Thus, social regulation is even more necessary in the case of an ecosystem externality. The model analyzes the changes in net present value of social welfare and farmers’ private benefits in the case of non cooperation and when cooperation prevails. In the presence of ecosystem externalities the incremental gains for a grand coalition may lead to creation of sub-coalitions that are preferred to the grand coalition. The ‘status quo’ is defined in this paper where farmers maximize the present value of their individual net present value of income/benefits. In the ‘status quo’ farmers neither internalize the water extractions affects on their neighbors’ income, nor the environmental externality. The cooperative solution is reached when farmers introduce in their maximization problem a function representing the environmental externality and the other farmers’ consumption. In this case it is expected to obtain lower private benefits and a decrease in farmers’ extractions, leading to a recovery in 3 the water table level. The social welfare is defined in the cooperative game, as the farmers’ private benefits plus the incremental improvement in the ecosystems due to the increase in the water level (private welfare plus external benefits). The model is applied to one of the most important aquifers in Spain-Eastern La Mancha aquifer. The overexploitation of this aquifer during the last 30 years is driving a significant depletion of the water table level. The case of this aquifer is also important due to be one of the few examples worldwide of an aquifer where cooperation between farmers is working successfully. This cooperation began in the mid 1990s mainly because pressure from downstream users and river basin authority to prohibit agriculture in this area. A theoretical and empirical framework is developed in the paper. Section 2 presents the game theory model. Section 3 describes the study area of the Eastern La Mancha aquifer and outlines the empirical model. Section 4 describes the results in the different scenarios and the effectiveness and stability of possible coalitions between farmers. Finally, section 5 concludes. 2. A game theory model applied to groundwater management with externalities Assume a CPR shared by π users, π =1, …, π½. For simplicity assume that each user is confined to a certain land area with given characteristics that affects both the performance of that user and also the performance of adjacent users (extraction externality). Assume that the users/players are placed sequentially such that player π borders only with player π − 1 and with player π + 1(and that if π = 1 it borders only with π + 1, and if π = π½ it borders only with π − 1). Assume that each player π uses the CPR for its own benefit. However, in doing so, player π inflicts negative extraction externalities on its neighbors π − 1 and π + 1. For example, in the case of groundwater, such multidirectional externalities could be in the form of a relative level of the water table. In addition, all players, through their aggregate action impose an externality on an ecosystem that is connected to the CPR and indirectly affects the players that are part of the society that benefits from the ecosystem services. Users of the CPR consider joint management options by agreeing on an optimal management plan over a long-term planning horizon, which can be 4 translated into a net present value of benefits. Therefore, any cooperative arrangement is referred to an allocation scheme of the present value of the sum of net benefits over the planning horizon. For simplicity and without loss of generality we will eliminate in the theoretical model the time variable and refer to the annual level of decisions and payoffs. Let π be the maximum level of the CPR. Player π uses π₯π ≤ π such that ∑π π₯π ≤ π and produces π¦π = ππ (π₯π , ∑π π₯π ; ∀π ≠ π ) with ππ¦π ππ₯π ≤ 0. The expression ππ¦π ππ₯π ππ¦π ππ₯π ≥ 0, π 2 π¦π ππ₯π 2 ≤ 0, and is the extraction externality. Let π be the set of the grand coalition players and π⊆π be the set of all possible partial coalitions. A partial coalitions π ⊆ π may include 2, 3, …, π½ − 1 members with the following characteristic functional forms: For a singleton coalitions {π}: ππ (π₯π , π₯π−1 , π₯π+1 ) ∀ π½ > π > 1 ππ (π₯π , π₯π−1 ) ∀ π = 1 ππ (π₯π , π₯π+1 ) ∀ π = π½ {π} π¦π ={ (1) For any coalition π the characteristic function will depend on the number of members in π and on the location of π in the CPR landscape. For a two member coalition {π, π + 1} the characteristic function is: {π,π+1} π¦2 π+1 =ππ (∑π π₯π ; π₯π+2 ) ∀ π = 1, 2, … , π½ − 1 (2) For a 3 player coalition: {π,π+1,π+2} π¦3 π+2 =ππ (∑π π₯π ; π₯π+3 ) ∀ π = 1, 2, … , π½ − 2 (3) . . . For a π½ − 1 player coalition: {π,π+1,…π½−1} π¦π½−1 =ππ (∑π½−1 π₯π ; π₯π½ ) ∀ π = 1, 2, … , π½ π (4) And for the grand coalition: {π} π¦π½ =ππ (∑π½π π₯π ) ∀ π = 1, 2, … , π½ (5) The environmental externality is a value function that connects between the remaining level of the CPR, π − ∑π½π π₯π , and the value of the ecosystem, πΈ. The lower the remaining level of the CPR the lower is the value of the ecosystem: πΈ = π(π − ∑π½π π₯π ), with: 5 ππΈ π ∑π½π π₯π <0 We postulate that | (6) ππΈ π½ π ∑π π₯π ππ¦ | β« |∑π ππ₯π |. Assume that a grand coalition solution π for the aquifer produces a value of π£(π) that needs to be divided among the players so that the following relationships hold. Assume that the allocation of the cooperative gains are divided among the players such that player π gets πΊπ . Each player has to be better off in the cooperative solution compared with the status quo (individual rationality). Thus, πΊπ ≥ π¦{π} ∀π ∈ π. Each player has also to be better of in the cooperative solution than in any partial coalition arrangement, fulfilling also the group rationality condition ∑π∈π πΊπ ≥ π¦{π } ∀π ⊂ π. And finally, the value of the entire set of players have to be fully allocated by the grand coalition participants, namely, ∑π∈π πΊπ = π¦{π}. An allocation that fulfills these three requirements is in the core of the game. 3. The Eastern La Mancha aquifer model Eastern La Mancha aquifer is one of the biggest aquifer in Spain. This aquifer extends over 7,200 km2, covering the regions of Albacete, Cuenca and Valencia. The aquifer is part of the Jucar River Basin Authority, representing an 18 per cent of the total area of the Basin (see Figure 1). The area has a Mediterranean weather characterized by important fluctuations in daily and seasonal temperatures, with cold winters and hot summers. The precipitations also register several seasonal fluctuations and vary between nearly 350 mm/year in the south to nearly 550 mm/year in the north. This groundwater is mostly used to irrigation agriculture (80% of the total water use), but also there is a slight consumption for urban (8% of total water use) and industrial activities (12% of total water use). During the 1970s and mainly due to the development of advanced and efficient irrigation technologies a significant increase in groundwater extraction took place. From the seventies the irrigated agriculture has extended to nearly 90,000 Hectares. During this period the pressure on the aquifer has largely increased, generating a significant over-exploitation. This over-exploitation is affecting, mostly in dry periods, the whole Jucar River system and the ecosystems linked to the aquifer. 6 Figure 1. Eastern La Mancha aquifer location Source: adapted from Martin de Santa Olalla et al. (2007) This paper models the cooperation in Eastern La Mancha, where farmers are currently cooperating to reduce their groundwater consumption (Esteban and Albiac 2010a,b). The Eastern La Mancha aquifer is linked with Jucar River. In some parts of the River the aquifer supplies water to the River but in other parts the River supplies water to the aquifer. Because the decrease in the water table level the contributions from the aquifer to the River decrease, increasing the flow from the River to the aquifer. Because the political pressure of farmers downstream, individuals in Albacete realized that if they do not reduce their extractions the whole agriculture in the area could be jeopardized. Therefore, cooperation was initiated in order to reduce the extractions to a sustainable level (recharge equal extractions). The paper assumes an aquifer area divided into three different sub-areas characterized by different water table depths, total area, irrigated area and cropping pattern, aquifer natural level3, and recharge. The model assumes that the farmers’ activity affects the ecosystems linked to the aquifer and also neighboring areas (environmental and extraction externalities respectively). Farmers in each sub-area can act individually, ignoring both the ecosystem and the effect of their extraction on their neighbors’ extractions. They can partially cooperate with their closer neighbor, internalizing the environmental externality and the extraction externality (in partial cooperation one region acts as ‘freerider’). The last option is full cooperation, where all farmers cooperate internalizing the entire externalities. 3 Aquifer level when non human interventions have been made. 7 3.1. Study area: sub-aquifers definition The aquifer is divided following the work of Castaño et al. (2010). Six different sub-aquifers can be defined: Northern Domain (ND) that is extended over 1,870 km2 and the irrigation surface is around 150 km 2; Central Domain (CD) spans over 3,600 km2 with an irrigated area of 670 km2; El Salobral-Los Llanos Domain (SLD) with an area of 400 km2 and 200 km2 of irrigation agriculture; Moro-Nevazos Domain (MND) with 520 km2 and an irrigation area of 300 km2; Pozocañada Domain (PCD) with 270 km2 of which 70 km2 are irrigated; finally Montearagón-Carcelén Domain (MCD) with 600 km2 which is not irrigated4. For simplicity in the model the last three areas located in the south of the aquifer (SLD, MND, and PCD) are lumped as South Domain, SD. Figure 2 shows the different parts of the aquifer. Figure 2. Eastern La Mancha aquifer sub-areas Source: adapted with some modifications from Castaño et al. 2010. The main crops are classified as spring, summer, and summer-spring. Spring crops are characterized by total revenue per hectare of 2,705 m 3/ha, the revenue of summer crops is 6,269 m3/ha, and finally spring-summer crops revenue is 7,415 m3/ha5 (Sanz et al. 2009, 2011). 3.2. Empirical model The empirical model is an optimal control problem that combines economic, agronomic and hydrologic variables. The farmers demand function is a fixed coefficient crop production function where each crop is characterized by fixed 4 5 The sub-area MCD is not included in the model because there is no irrigation. The main crop in spring is wheat, in summer is onion and corn, and alfalfa in summer-spring. 8 yields water requirements π€π and a revenue per unit of land ππ . Where the index π = π π, π π’, and π π , represents the crops (spring, summer, and summer-spring respectively). Farmers decide on how much land to allocate to each crop, so the groundwater consumption. The total number of hectares/year, per crop and π area, is defined as βππ (π‘), where the indexes represent the different aquifer areas (π = πΆπ·, ππ·, ππ·) and crop types. A Leontief crop production technology is assumed, where the inverse demand is a discontinuous function. The demand function depends on the available land area and the net income per land unit of each crop. Farmers’ annual private revenues are the per hectare crop-level revenue multiplied by the area per each crop: π π π΅ π [βππ (π‘), π‘] = ∑ ππ β βππ (π‘) (6) π π where π΅ π [βππ (π‘), π‘] is the revenue function, and ππ is the crop revenue per hectare. Revenues are defined as the fix quantity of water requirement per crop (π€π ) multiplied by crop prices (ππ ), so ππ = π€π β ππ . The annual production costs function by each area is the water extraction costs plus fixed costs per hectare6: π π πΆπ [βππ (π‘), π» π (π‘), π‘] = πΆ0 β ∑ βππ (π‘) π π + πΆ1 β (ππΏπ − π» π (π‘)) β ∑ βππ (π‘) β π€π (7) π where πΆ0 is the fixed pumping cost per hectare which is multiplied by the total irrigated acreage, and πΆ1 is the per unit of water constant marginal costs of pumping. The term πΆ1 is multiplied by the height of pumping, and by the total water pumped to cover irrigated acreage. The pumping height is given by the difference between the surface level of the aquifer (natural level) ππΏπ and the actual water table level π» π (π‘) in each sub-region. The water extractions per hectare for spring, summer and summer-spring crops are given by parameter π€π . The pumping costs per cubic meter are driven by the height of the water table, which is the difference between the natural and the water table levels in each sub-aquifer. 6 The model does not include other production costs (neither fix nor variable) as labor, other input costs, amortization, or machinery costs. 9 The farmers’ annual private gross margin is defined as the difference between the farmers’ annual revenue and the annual extraction cost (equation 6 minus equation 7). This is the result under the ‘status quo’, where farmers maximize their private gross margin ignoring that their water use affects the ecosystems and neighbors farmers. π π π πΊππ [βππ (π‘), π» π (π‘), π‘] = π΅ π [βππ (π‘), π‘] − πΆ[βππ (π‘), π» π (π‘), π‘] (8) The damages to ecosystem are caused by the fall in the water table and the progressive reduction in the flows that feed aquatic ecosystems. These damages are assumed here to be linear in the meters of aquifer reduction, which can be expressed also as the volume of the aquifer depletion. They are computed as the product of two terms: the damage per cubic meter of aquifer water depleted π½, multiplied by the meters of aquifer depletion (ππΏπ − π» π (π‘)). The annual ecosystem damages are given by the following expression: π· π [ π» π (π‘), π‘] = π½ β [ππΏπ − π» π (π‘)] (9) The farmers’ problem can be formulated as the maximization of the private gross margin. The dynamic problem is as follows: π π πππ₯ πΉπ = ∑ π‘=0 1 β [π΅ π [βπ π (π‘), π‘] − πΆ[βπ π (π‘), π» π (π‘), π‘] ] (1 + π)π‘ π π . π‘. π»Μ π = π π + (πΌ − 1) β ∑π βππ β π€π π΄π π π» π (0) = π»0π (10) where πππ₯ πΉππ maximizes the farmers’ private gross margin over the planning period subject to the hydrological behavior of the water flowing into the aquifer, and the water table level initial value7. r is the discount rate, π»Μ π is the change in the water table level over time π‘ (π»Μ π = π» π (π‘ + 1) − π» π (π‘)). π π is the natural recharge of the aquifer8. The parameter πΌ is the return flow coefficient (the water that returns to the aquifer due to water leaching and percolation). π΄ππ is the aquifer area multiplied by the aquifer storativity coefficient. The total water π extractions are represented by equation ∑π βππ β π€π . The total water extractions Water stock at the first period (π‘ = 0). This model assumes a fix recharge during the time. This is a simplification of the model because the recharge depends on stochastic elements like weather, soil, type of crops, irrigation technology, etc. The recharge is different in each sub-region. 7 8 10 multiplied by (1 − πΌ) is the total water from extractions that return to the aquifer (with πΌ representing the irrigation technology efficiency). When farmer π internalizes the entire externalities (environmental and extraction) of their activity the problem becomes: π π πππ₯ πΉππΈ = ∑ π‘=0 1 β [π΅ π [βπ π (π‘), π‘] − πΆ[βπ π (π‘), π» π (π‘), π‘] − π· π [ π» π (π‘), π‘] ] (1 + π)π‘ π π . π‘. π»Μ π = π π + (πΌ − 1) β ∑π βππ β π€π π΄π π π−1 + [π»0 π−1 −π π−1 π π−1 + (πΌ − 1) β ∑π βππ β π΄ππ−1 β π€π ] π» π (0) = π»0π (11) where the π − 1 represents the neighbor sub-aquifer that is being affected by farmers in region π consumption. The parameter π»0π−1 is the initial water table level in region π − 1, π π−1 shows the impact of the neighbor groundwater consumption in region π. This value is calculating with the total water consumption in region π − 1, the weight is calculating dividing the total extractions in region π − 1 by the aquifer area, π π−1 π π−1 +(πΌ−1)β∑π βππ π΄π π−1 βπ€π π−1 π−1 = ∑π βππ βπ€π π΄π π−1 , finally represents the extractions in region π − 19 (Gura and Maschler 2008:173-189). 4. Numerical application to the Eastern La Mancha aquifer Different scenarios have been run by a period horizon of 50 years using the program GAMS with the solver CONOPT. Farmers’ gross income, social welfare, and environmental damages are reported. The parameters used in the simulations are shown is Table 1. Two main scenarios are simulated: in the first one farmers do not internalize the environmental externality that their activity generates to the ecosystems; in the second scenario, farmers internalize the environmental externality introducing the ecosystem damage function into their optimization problem. An additional scenario with a sensitivity analysis has been simulated in order to 9 In the case of region CD which is being affected by both neighboring ND and SD regions, the externality should include both π + 1 and π − 1. 11 show the effect of different economic values of ecosystem in the coalitions’ stability. Table 1. Aquifer parameters Parameters Description Value (units) Intercept of the pumping function cost 340 (€/ha) πΆ0 Increase in costs of pumping a cubic meter, per meter πΆ1 0.0025 (€/m3βm) of decline in water table Return flow coefficient Social discount rate Value of water for ecosystems (damage of depletion)* Water requirements of spring crops Water requirements of summer crops Water requirements of spring-summer crops Crop revenue of spring crops Crop revenue of summer crops Crop revenue of spring-summer crops Water table natural level above sea level ND Water table natural level above sea level CD Water table natural level above sea level SD Current water table elevation above sea level in ND Current water table elevation above sea level in CD Current water table elevation above sea level in SD Recharge without irrigation return flows ND Recharge without irrigation return flows CD Recharge without irrigation return flows SD Area of the aquifer times storativity in ND Area of the aquifer times storativity in CD Area of the aquifer times storativity in SD πΌ π π½ π€π π π€π π’ π€π π ππ π ππ π’ ππ π ππΏππ· ππΏπΆπ· ππΏππ· π»0ππ· π»0πΆπ· π»0ππ· π ππ· π πΆπ· π ππ· π΄π ππ· π΄π πΆπ· π΄π ππ· Source: Sanz et al. (2009, 2011) and Judez et al. (2000, 2002)10 0.2 0.05 50,000 (€/m) 2,705 (m3/ha) 6,259 (m3/ha) 7,415 (m3/ha) 544 (€/ha) 2,500 (€/ha) 1,300 (€/ha) 680 (m) 660 (m) 670 (m) 650 (m) 635 (m) 640 (m) 75 (hm3) 150 (hm3) 95 (hm3) 59.84 (km2) 115.6 (km2) 38.08 (km2) By each scenario different simulations have been run: i) ‘status quo’, where farmers maximize their private gross income without internalizing any externality, either the extraction externality; ii) partial cooperation, farmers cooperate in groups of two11 (with the closer neighbor) internalizing both the 10 The economic value of the ecosystems has been approximated using the studies by Judez et al. (2000, 2002). These authors calculate the economic value of the wetland “Tablas de Daimiel” (National Park in Spain). This ecosystem is being affected by the decrease in the water table level of the Western La Mancha aquifer. Similarly to what happen in “Tablas de Daimiel”, several wetlands are also being affected in the case of Eastern La Mancha. The depletion of the aquifer is affecting the survival of some ecosystems in this area. Due to the lack of information about the economic value of the wetlands in this region we are using as an approximation the value calculated to “Tablas de Daimiel”. A sensitivity analysis is made in the empirical application in order to check the results with different economic values of ecosystems. 11 The third region, not into the coalition, acts as ‘free-rider’ without internalizing any externality, neither environmental nor extraction. 12 environmental and the extraction externalities; iii) full cooperation, coalition between the three regions where the entire environmental and extraction externalities are internalized. 4.1. Analysis of results In the first baseline (status quo) scenario, farmers do not internalize the effect of their activity on the ecosystems that are linked with the aquifer. In the ‘status quo’ non externality is internalized and each region acts separately. In partial cooperation and full cooperation, the extraction externality is taken into account but the environmental externality is ignored by all coalitions. The results of this scenario are presented in Table 2. Table 2. Baseline simulation: ‘status quo’, partial cooperation and full cooperation when farmers do not internalize the environmental externality ‘Status quo’ Variable ND CD SD Environmental damage (€/year)* Gross margin (€/year)* Social welfare (€/year)* Variable 40.09 1,801.73 1,759.54 Partial cooperation ND and CD ND+CD Environmental damage (€/year)* Gross margin (€/year)* Social welfare (€/year)* Variable 54.25 753.70 699.30 94.34 2,556.61 2,462.41 Partial cooperation CD and SD ND Environmental damage (€/year)* Gross margin (€/year)* Social welfare (€/year)* Variable Environmental damage (€/year)* Gross margin (€/year)* Social welfare (€/year)* * Data in million Euros 54.25 753.70 699.30 48.69 2,562.71 2,512.59 SD 48.69 2,562.71 2,512.59 CD+SD 88.71 4,375.53 4,288.27 Full cooperation ND+CD+SD 142.96 5,130.41 4,991.15 The results suggest that partial or full cooperation achieves highest levels of gross margin. The best results are achieved in the simulation of full cooperation, demonstrating that when farmers decide to cooperate, all increase their private benefits. In a similar way the social welfare increases when cooperation between farmers takes place. The highest social welfare is reached in full cooperation and the lowest is reached in the ‘status quo’. Partial cooperation 13 between CD and SD is always preferred than partial cooperation between ND and CD (in terms of social welfare, gross margin, and environmental damage). Table 3 presents the results when farmers internalize the environmental externality of their activity. The model assumes that for any type of cooperation, farmers internalize the environmental externality, while in the ‘status quo’ farmers continue ignoring this damage12. When partial cooperation exists the region that is no cooperating does not internalize any of the externalities. Table 3. Results of the ‘status quo’, partial cooperation and full cooperation when farmers internalize the environmental externality** ‘Status quo’ Variable ND CD SD Environmental damage (€/year)* Gross margin (€/year)* Social welfare (€/year)* Variable 91.14 2,488.78 2,580.09 Partial cooperation CD and SD ND Environmental damage (€/year)* Gross margin (€/year)* Social welfare (€/year)* Variable 40.09 1,801.73 1,759.54 48.69 2,562.71 2,512.59 Partial cooperation ND and CD ND+CD Environmental damage (€/year)* Gross margin (€/year)* Social welfare (€/year)* Variable 54.25 753.70 699.30 54.25 753.70 699.30 SD 48.69 2,562.71 2,512.59 CD+SD 85.27 4,313.33 4,400.14 Full cooperation ND+CD+SD Environmental damage (€/year)* 137.55 Gross margin (€/year)* 4,982.48 Social welfare (€/year)* 5,123.90 * Data in million Euros ** The value of the environmental externality is 50,000€ per meter of aquifer depletion or replenishment. When the environmental externality is internalized the social welfare increases, in all the cooperative simulations, compares with the baseline scenario. On the other hand, the gross margin decreases, also in the three cooperation simulations, due to the increase in the farmers’ internalization costs. The highest social welfare is achieved when full cooperation exists. In the case of partial cooperation, the best social welfare is reached when CD and SD regions cooperate. The results are different when we analyze the gross margin. The highest gross margin is reached in the ‘status quo’ due to non 12 The results of the ‘status quo’ are equal to the ones obtained in the baseline scenario. 14 internalization of any externality by the farmers. But when cooperation exists, partial cooperation yields better payoffs than full cooperation, and cooperation between regions ND and CD is superior to that between CD and SD (more efficient in social welfare terms)13. The last scenario illustrates a sensitivity analysis using different economic values for the environmental externality. The values used are half and double of the ecosystem value assigned in the previous scenario (Table 3). The results are shown in Table 4. The results in the sensitivity analysis corroborate the ones obtained in the previous scenario. In the case of a small value of ecosystem damages (25,000€ per meter of depletion) the highest value of social welfare is achieved by the full cooperation. Partial cooperation between CD and SD regions has also a higher social welfare than the coalition between ND and CD regions. But in the case of the gross margin, the highest value is achieved with the coalition between CD and ND. The gross margin in this case is even higher than the ‘status quo’ one. With a small value of ecosystem damage partial cooperation is preferred over individual coalitions in the Status Quo. In the case of a higher value of environmental damages (100,000€ per meter of depletion) the results replicate the ones obtained in the previous scenario. The highest social welfare is reached under full cooperation and the lowest in the ‘status quo’. The social welfare in the coalition between CD and SD regions is higher than the one in the coalition between ND and CD. The highest gross margin is in the ‘status quo’ one, followed by the coalition between CD and SD. The lowest one is achieved in the full cooperation because all farmers are internalizing the environmental externality. In partial cooperation simulations the ‘free-rider’ region does not internalize the environmental externality. This fact generates a higher gross margin in partial cooperation compare with full cooperation. So, the total gross margin is higher with partial cooperation rather than with full cooperation. 13 15 Table 4. Sensitivity analysis: results of the ‘status quo’, partial cooperation and full cooperation with different values of environmental damages** SENSITIVITY ANALYSIS: VALUE ECOSYSTEMS 25,000 €/m ‘Status quo’ Variable ND CD SD Environmental damage (€/year)* Gross margin (€/year)* Social welfare (€/year)* Variable 20.04 1,801.73 1,779.58 Partial cooperation ND and CD ND+CD Environmental damage (€/year)* Gross margin (€/year)* Social welfare (€/year)* Variable 27.13 753.70 726.42 46.46 2,540.74 2,587.31 27.13 753.70 726.42 Environmental damage (€/year)* Gross margin (€/year)* Social welfare (€/year)* 44.51 4,374.29 4,420.35 70.28 5,110.25 5,184.71 SENSITIVITY ANALYSIS: VALUE ECOSYSTEMS 100,000 €/m ‘Status quo’ Variable ND CD Environmental damage (€/year)* Gross margin (€/year)* Social welfare (€/year)* 80.18 1,801.73 1,719.45 175.42 2,376.47 2,552.07 Partial cooperation CD and SD ND Environmental damage (€/year)* Gross margin (€/year)* Social welfare (€/year)* Variable 108.51 753.70 645.04 Partial cooperation ND and CD ND+CD Environmental damage (€/year)* Gross margin (€/year)* Social welfare (€/year)* Variable CD+SD Full cooperation ND+CD+SD Variable Variable SD 24.34 2,562.71 2,536.93 Partial cooperation CD and SD ND Environmental damage (€/year)* Gross margin (€/year)* Social welfare (€/year)* 24.34 2,562.71 2,536.93 108.51 753.70 645.04 SD 97.38 2,562.71 2,463.89 SD 97.38 2,562.71 2,463.89 CD+SD 163.45 4,232.58 4,397.75 Full cooperation ND+CD+SD Environmental damage (€/year)* 264.53 Gross margin (€/year)* 4,863.44 Social welfare (€/year)* 5,132.23 * Data in million Euros ** The value of the environmental externality is per meter of aquifer depletion or replenishment. 16 4.2. Game theory allocations We apply a couple of game theory allocation solution concepts to the aquifer management problem, referring mainly to the results in Tables 2, 3, and 4. Two cooperative game theory allocation schemes, the Nash-Harsanyi solution and the Shapley Value are applied. Once we calculate the resulting allocations of the full cooperation payoff among the three regions, we test for their inclusion in the Core, which is one of the conditions for stability, and also apply the Loheman Power Index, which is a proxy for stability of an allocation scheme (for more explanation see Dinar et al. 2007:122-131). The Shapley Value (πΊπ ) is calculated, based on the incremental contributions of the players to the grand coalition. The Nash-Harsanyi allocation (π©π ) is calculated, by maximizing the grand coalition’s members incremental payoff, based on an equal incremental allocation of the total cooperative payoff (compared with the status quo) to all players. We start with calculations of the Nash-Harsanyi allocation, which is presented in Table 5. Table 5. Nash-Harsanyi allocation of the cooperative payoffs Variable No internalization of externality Internalization of externality (50,000 €/m) Internalization of externality (25,000 €/m) Internalization of externality, value of externality 100,000 Gross Margin ND+CD+SD NDCDSD Difference Incremental gains above status Allocation of cooperation payoff Core conditions 5116 5130 14 5116 4982 -134 5116 5110 -6 5116 4863 253 4.65 N/A NA 84.33 {757.65, 1805.65, 2566.65} In the Core N/A N/A Not in the Core Not in the Core {837.33, 1885.33, 2646.33} Not in the Core Social Welfare ND+CD+SD NDCDSD Difference Incremental gains above status N-H Allocation of cooperation payoff Core conditions 4970 4991 21 4970 5123 153 5041 5184 143 4827 5132 305 7 51 47.66 101.66 {706, 1766, 2519} In the Core {750, 1810, 2563} {773.66, 1826.66, 2583.66} In the Core {746.66, 1820.66, 2564.66} In the Core In the Core As can be seen from Table 5 allocation of the gross margin doesn’t allow always having incremental benefits, especially when the value of the environmental externality is relatively low. In addition, the grand coalition values are always higher in the case of the social welfare calculations 17 compared with the case of the gross margin calculations. In the case of using the social welfare, the cooperation benefits are the highest when the value of the environmental externalities is the lowest. In the case the Shapley Value we report the cooperation allocations and in addition we calculate measures of stability of the solution. Table 6 provides the results of such analyses. Shapley value calculations suggest that in the case of the gross margin the Shapley Value did not yield results that are in the Core for scenarios of the two lower values of the environmental externality (25,000€ and 50,000€). All the rest of the scenarios Sahpley Value allocations are in the core. In addition, the Loehman Power Index can be presented in terms of Coefficient of Variation (CV) of the set of individual Power Indexes with higher values of CV indicating less stability. The results in Table 5 suggest that the allocation solutions for the Social welfare scenarios are more stable than those for the gross margin. In addition, stability of the Shapley solution decreases as the value of the environmental externality increases. Table 6. Shapley Value Allocations and Stability measures Variable No internalization of externality Internalization of externality, value of externality 50,000 E Internalization of externality, value of externality 25,000 E Internalization of externality, value of externality 100,000 E Gross Margin Shapley Allocation of cooperative payoff Core conditions CV of Loehman Power Index/Stability {754, 1808, 2568} {714, 1737, 2531} {745, 1799, 2567 } {683, 1665, 2515} In the Core Not in the Core Not in the Core In the Core 0.71 N/A N/A 0.55 Social Welfare Shapley Allocation of cooperative payoff Core conditions CV of Loehman Power Index/Stability {701, 1770, 2521} {727, 1852, 2544} {784, 1817, 2583} {691, 1873, 2568} In the Core In the Core In the Core In the Core 0.63 0.71 0.22 0.53 5. Summary and Conclusions Common pool resources (CPRs) are goods with the characteristics of ‘openaccess’ and non rivalry in the consumption until congestion affects the resource availability, leading to scarcity. Additionally, negative externalities may be involved in the use of such resources. A typical example of CPR is groundwater 18 used for irrigation purposes. Due to the significant development of irrigated agriculture worldwide and the exponential growth of world population during the last century the pressure on water resources has largely increased. This pressure creates several problems of water contamination and water scarcity. This paper focuses on the study of groundwater management, which traditionally was unregulated, leading to problems of overexploitation. Due to the overexploitation, two main externalities can be identified, environmental externalities (impacts on ecosystems linked to the aquifer) and extractions externalities (impacts on other groundwater users). The paper develops a model of an aquifer, which is divided into three different regions; each region extracts water for irrigation purposes, generating both externalities. The model analyzes the propensity for cooperation between regions under scenarios of internalizing and not internalizing the different externalities. An empirically application of the model is carried out in one of the most important aquifers in Spain, the Eastern La Mancha aquifer. The results of the analysis suggest that when environmental externalities are not accounted for by players, the grand coalition is the preferred result. Farmers and society are always better of when there is cooperation (partial or full) than when farmers acts individually. But, when the environmental externalities are accounted for the results may be less obvious. When regions/plyers internalize the environmental externality the incentives to cooperate decrease; the higher the environmental damage the lower the incentives to cooperate. Even though in terms of social welfare the preferred option is the full cooperation, the Core becomes smaller. These results are supported by some game theory allocation solutions (Nash-Harsanyi and Shapley value). Additionally, some stability measures have been calculated (Loheman Power Index). These measures suggest that social welfare considerations lead to more stable than gross margin ones. The stability of the possible coalitions decreases as the value of the ecosystems’ damage increases. Without environmental externalities famers have incentives to cooperate due to an increase in their private gross margin, and the society welfare increases as well. However, as soon as the environmental externalities are introduced the farmers’ gross margin incentives associated with cooperation disappear. 19 Acknowledgements This paper was prepared while the first author was a post doc researcher at the Water Science and Policy Center, University of California, Riverside. The authors appreciate the assistance of David Sanz (Instituto de Desarrollo Regional, University of Castilla la Mancha, Spain) for his valuable help with the agronomic data and hydrological information. References Anderson, G., J. Opaluch and W.M. Sullivan. (1985). “Nonpoint agricultural pollution: pesticide contamination of groundwater supplies”. American Journal of Agricultural Economics 67, 1238-1246. Castaño, S., D. Sanz and J.J. Gómez-Alday. (2010). “Methodology for quantifying groundwater abstractions for agricultura via remote sensing and GIS”. Water Resource Management 24, 795-814. Coase, R. (1960). “The problem of social cost”. Journal of Law and Economics 3, 1-44. Custodio, E. (2002). “Aquifer overexploitation: what does it mean?”. Hydrogeology Journal 10, 254-277. Dinar, A. (1994). “Impact of energy costs and water resource availability on agriculture and groundwater quality in California”. Resource and Energy Economics 16, 47-66. Dinar, A. and A. Xepapadeas. (1998). “Regulating water quantity and quality in irrigated agriculture”. Journal of Environmental Economics and Management 54, 273-290. Dinar, A., S. Dinar, S. McCaffrey and D. McKinney. (2007). Bridges over Water: Understanding Transboundary Water Conflicts, Negotiation and Cooperation. World Scientific Publishers. Dufournaud, C.M. and J.J. Harrington. (1990). “Temporal and spatial distribution of benefits and costs in river-basin schemes: a cooperative game approach”. Environmental and Planning 22, 615-628. Esteban, E. and J. Albiac. (2010a). “Groundwater and Ecosystems Management: Analytical Findings”. Working Paper No 10/02. Department of Agricultural Economics, CITA, DGA, Zaragoza. Available at: Available at: www.unizar.es/econatura/documentos/recursoshidricos/wd1002.pdf 20 Esteban, E. and J. Albiac. (2010b). “Groundwater and Ecosystems Management: Empirical Findings from La Mancha Aquifers”. Working Paper No 10/03, Department of Agricultural Economics, CITA-DGA, Zaragoza. Available at: www.unizar.es/econatura/documentos/recursoshidricos/wd1003.pdf Gisser, M., and D.A. Sánchez. (1980). “Competition versus optimal control in groundwater pumping”. Water Resource Research 16 (4), 638-642. Gordon, H.S. (1954). “The economic theory of a common pool property resource: The fishery”. Journal of Political Economy 62, 124-142. Gura, E.Y. and M.B. Maschler. (2008). Insights into game theory. An alternative mathematical experience. Cambridge University Press. Iglesias-Martínez, E. (2002). “La gestión de las aguas subterráneas en el acuíferos Mancha Occidental”. Economía Agraria y Recursos Naturales 2, 69-88. Judez, L., R. de Andrés, C. Pérez-Hugalde, E. Urzainqui and M. Ibáñez. (2000). “Influence of bid and subsample vector son the welfare measure estimate in dichotomous choice contingent valuation: evidence from a casestudy”. Journal of Environmental Management 60, 253-265. Judez, L., M. Ibáñez, C. Pérez-Hugalde, R. de Andrés, E. Urzainqui and J. Fuentes-Pila. (2002). “Valoración del uso recreativo de un humedal español. Test y comparación de diferentes métodos de valoración”. Revista de Estudios Agrosociales y Pesqueros 192, 83-104. Koundouri, P. (2004). “Current issues in the economics of groundwater resource management”. Journal of Economic Surveys 18 (5), 703-738. Llamas, R. (1998). “Conflics between wetland conservation and groundwater exploitation: two case histories in Spain“. Environmental Geology Water Science 11, 241-251. Madani, K. and A. Dinar. (2011). “Cooperative Institutions for Sustainable Management of Common Pool Resources”. Water Science and Policy Center Working Paper 02-0311. Available at: http://wspc.ucr.edu/WSPC_WP_02_0311%20coop%20inst%20com%20pool.pdf. Martín de Santa Olalla, F., A. Domínguez, F. Ortega, A. Artigao and C. Fabeiro. (2007). “Bayesian networks in planning a large aquifer in Eastern Mancha, Spain”. Environmental Modelling & Software 22, 1089-1100. 21 Martínez-Santos, P., L. de Stefano, M.R. Llamas and P.E. Martínez-Alfaro. (2008). “Wetland restoiration in the Mancha Occidental aquifer, Spain: a critical perspective on water, agricultural, and environmental policies”. Restoration Ecology 16, 511-521. Milliman, J.W. (1956). “Commonality, the price system, and use of water supplies”. Southern Economic Journal 22, 426-437. Negri, D.H. (1989). “The common property aquifer as a differential game”. Water Resource Research 25, 9-15. Ostrom, E. (1990). Governing the Commons: The Evolution of Institutions for Collective Action. Cambridge University Press, Cambridge. Ostrom, E. (2010). Beyond markets and states: Polycentric governance of complex economic systems. American Economic Review 100, 641-672. Pigou, A. (1920). The Economics of Welfare. Macmillan, New York. Roseta-Palma, C. (2002). “Groundwater management and endogenous water quality”. Journal of Environmental Economics and Management 44, 93-105. Polansky, S., N. Tarui, G.M. Ellis and C.F. Mason. (2006). “Cooperation in the commons”. Economic Theory 29, 71-88. Provencher, B. and O. Burt. (1993). “The externalities associated with the common property exploitation of groundwater”. Journal of Environmental Economics and Management 24, 139-158. Rubio, J.S. and B. Casino. (2001). “Competitive versus efficient extracion of a common property resource: The groundwater case”. Journal of Economics Dynamics & Control 25, 1117-1137. Sanz, D., J.J. Gómez-Alday, S. Castaño, A. Moratalla, J. de las Heras, P.E. Martínez-Alfaro. (2009). “Hydrostratigraphic framework and hydrogeolocigal behaviour of the Mancha Oriental System (SE Spain)”. Hydrogeology Journal 17, 1375-1391. Sanz, D., S. Castaño, E. Cassiraga, A. Sahuquillo, J.J. Gómez-Alday, S. Peña and A. Calera. (2011). “Modeling aquifer-river interactions under the influence of groundwater abstractions in the Mancha Oriental System (SE Spain)”. Hydrogeology Journal 19, 475-487. Tarui, N., C.F. Mason, S. Polansky and G. Ellis. (2008). “Cooperation in the commons with unobservable actions”. Journal of Environmental Economics and Management 55, 37-51. 22 Tsur, Y. (1990). “Stabilization role of groundwater when surface water supplies are uncertain: the implications for groundwater development”. Water Resource Research 26, 811-818. Tsur, Y. and A. Zemel. (1995). “Uncertainty and irreversibility in groundwater resource management”. Journal of Environmental Economics and Management 29, 149-161. Yadav, S. (1997). “Dynamic optimization of nitrogen use when groundwater contamination is internalized at the standard in the long run”. American Journal of Agricultural Economics 79, 931-945. 23