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Tecnología y ciencias del agua

versión On-line ISSN 2007-2422

Tecnol. cienc. agua vol.10 no.5 Jiutepec sep./oct. 2019  Epub 15-Feb-2020 


Effects of climate change on hydrological planning: Proposal actions in the Guadalhorce River Basin

Efectos del cambio climático en la planificación hidrológica: propuesta de actuación en la cuenca del río Guadalhorce

Pedro Jiménez-Fernández1 

Alberto Jiménez-Madrid2 

German Gemár3

1Universidad de Málaga/PROAMB Integrada, Málaga, España,

2PROAMB Integrada, España/Technical University of Civil Engineering of Bucharest, Bucharest, Rumania,

3Universidad de Málaga, Málaga, España,


The Fifth Assessment Report from the Intergovernmental Panel on Climate Change estimates an increase in average temperatures and a 10-20% precipitation decrease for the Mediterranean region, which will likely generate drought events in the Guadalorce River watershed. This study attempts to determinate the potential impacts that climate change may have on water resources. The Guadalhorce River basin is the most important in Malaga (southern region of Spain) and supplies water to more than 10 000 ha of crops and Malaga city. The degree to which climate change-driven droughts will alter water resource supplies and demands were evaluated. Resulting social and environmental implications were also determined.

Keywords: Guadalhorce River; hydrological planning; climate change; water resource; governance


El Quinto Informe de Evaluación del Panel Intergubernamental sobre Cambio Climático estima un aumento en las temperaturas y una disminución de precipitación entre 10 y 20% para la región mediterránea, que podría generar eventos de sequía en el área de investigación. Este trabajo trata de determinar los impactos potenciales que el cambio climático puede tener en los recursos hídricos. La cuenca del río Guadalhorce es la más importante en Málaga (sur de España) y abastece de agua a más de 10 000 ha de cultivos y a la ciudad de Málaga. Se ha evaluado el grado de los efectos a los recursos hídricos frente a los episodios de sequía, y las implicaciones sociales y ambientales que resultarán.

Palabras clave: río Guadalhorce; planificación hidrológica; cambio climático; recurso hídrico; gobierno


Water is the most abundant liquid on Earth. Water represents the most important natural resource and the basis of all life. Given the importance of water for living organisms and due to the increasing pressures of growth on demand for good quality and sufficient quantities of water for all uses, it is necessary to enact measures encouraging water protection in qualitative and quantitative terms to guarantee its sustainability (European Union, 2000). Mediterranean regions are characterized by low and concentrated rainfall in the spring and autumn seasons, and by very hot temperatures in summer and mild temperatures in winter. Therefore, water is a clear limiting factor for many natural and human activities in Mediterranean habitats.

In 1961, the first Coordinated Plan for Guadalhorce Project was approved to guarantee the water demands of the irrigated area of the lower Guadalhorce River basin and the supply of drinking water to the city of Malaga (n.a., 1961). This project contemplated the irrigation of 19 032 ha, which led to a study of resource exploitation throughout the full Guadalhorce River and its tributaries. This study included a preliminary project for a reservoir on the Guadalhorce River and Guadalteba River complementary to the existing one on the Turon River (reservoir of Conde del Guadalhorce), and which currently make up the system of exploitation of Guadalhorce´s Dams, as well as diversion channels, irrigation channels on both banks of the river, hydroelectric jumps, creation of new population centres, drinking water supply to Málaga, works of channelling and defence of margins, and others.

Subsequently, in 1972, the new Coordinated Plan was approved (n.a., 1972). This update contemplated the irrigation of 21 621 ha, although the affected area was situated around 13 000 ha, whereas only about 10 000 ha have been irrigated (Table 1).

Table 1 Modification of land area in the different Coordinated Plans. 

Date Irrigated area (ha) Surface collection (ha)
1900 ≈ 5 000 --
1961 ≈ 9 000 19 032
1972 10 135 21 621

Resources from the exploitation of the Guadalhorce River system provide the main source of drinking water for Malaga city, which consisted of almost 570 000 inhabitants in 2015. This system is located about 65 km from the capital in-between the municipalities of Alora, Antequera, Ardales, Campillos, and Teba. Its management is of great importance for Malaga and its conurbation.

The Guadalhorce Valley Irrigation Area is located in the south of the province of Malaga, close to its capital (Figure 1). It coincides geographically with the valley of the same name river and covers lands belonging to the municipalities of Alhaurin el Grande, Alhaurin de la Torre, Alora, Cartama, Casarabonela, Coin, Malaga, and Pizarra.

Figure 1 Location of the research area. 

Determining the potential impacts of climate change on water resources is complicated because of limited data availability for calibrating models, and because of the high exploitation rate (the relation between the available resource and the degree of artificial use) of the water bodies in the research region. These conditions make modeling under natural system operating conditions almost impossible.

Having models that reflect the actual functioning of a water system becomes essential for the effective management of the water resources in a basin while taking into account the different scenarios of climate change predicted by the Intergovernmental Panel on Climate Change (IPCC) in their AR5 report, which estimates increased average temperatures and an overall 10-30% decrease in rainfall for the Mediterranean region (Jiménez-Gavilán & Jiménez-Fernández, 2015).

The objective of this work was to determine the effects of climate change on water resources and associated hydrological planning needs, as well as to evaluate the social and environmental implications of future drought episodes. Finally, from a hydrological point of view, the research area is included within the Hydrographic Demarcation of the Andalusian Mediterranean Basins (HDAMB), whose Hydrological Plan was approved in January, 2016. It contains forecasts of demands for, and sources of, resources for the next planning horizons to meet the environmental objectives in the area as set out in the Water Framework Directive (2021 and 2027).


Bibliographic compilation

All information concerning the characterization of the research area, primarily related to water resources management, was collected and analyzed (Sánchez-García, 2010; Jiménez-Fernández, 2010; Jiménez-Gavilán, Jiménez-Fernández, Morales-Calvo, & Ruiz-Antúnez, 2013). Data for the different scenarios of climate change from the IPCC AR5 for the Mediterranean area were used, with particular emphasis on the scenarios RCP4.5 and RCP8.5 (Table 2).

Table 2 Temperature and precipitation change in Mediterranean region (Stocker et al., 2014). 

Period Temperature change (ºC)
2016-2035 2046-2065 2081-2100 2016-2035 2046-2065 2081-2100
RCP4.5 RCP4.5 RCP4.5 RCP8.5 RCP8.5 RCP8.5
Dec-Feb 1 2 2 1 3 4
Mar-May 1.5 2 3 1.5 3 5
Jun-Aug 1.5 3 3 2 4 7
Sep-Nov 1.5 2 3 1.5 3 5
Period Precipitation change (%)
RCP4.5 RCP4.5 RCP4.5 RCP8.5 RCP8.5 RCP8.5
Oct-Mar 0 -10 -10 0 -10 -20
April-Sep -10 -10 -10 0 -20 -30

Updating the irrigation area

An inventory and mapping of the whole irrigable area with the subsequent characterization of terrain was performed previously through photointerpretation and cartography in the Inventory and Characterization of the Irrigated Area of Andalusia (ICRA, 2008). This cartography considered both irrigated and non-irrigated areas and the main crop type grown in each plot that makes up the irrigated area (Table 3).

Table 3 Percentage of irrigated area planted in specific crop types. 

Crop Percentage (%)
Citrus crops 60.94
Extensive winter 1.00
Fruit trees 16.30
Vegetable fields 13.90
Olive field 6.10
Other 1.76
Total 100.00

Climate change

The IPCC published their Fifth Assessment Report (AR5) in October 2014 that defines the latest climate change scenarios estimated by this agency. The scenarios used by Working Group I of the IPCC focused on anthropogenic emissions and did not include changes in natural drivers, such as solar or volcanic forcing or natural emissions of, for example, CH4 and N2O (Stocker et al., 2014). For AR5, the scientific community defined a set of four new scenarios, called Representative Concentration Pathways (RCP), which are characterized by the approximate calculation that these scenarios make for total radiative forcing in the year 2100 in relation to 1750, that is to say, 2.6 W m-2 for scenario RCP2.6, 4.5 W m-2 for scenario RCP4.5, 6.0 W m-2 for scenario RCP6.0, and 8.5 W m-2 for scenario RCP8.5 (Stocker et al., 2014). The four RCP scenarios comprise a mitigation scenario leading to a very low level of forcing (RCP2.6), two stabilization scenarios (RCP4.5 and RCP6.0), and a scenario with a very high level of greenhouse gas emissions (RCP8.5). Consequently, RCP scenarios represent a variety of 21st century climate policies, compared to the scenarios of the Special Report on Emission Scenarios (SRES), which did not include climate policies, used in the Third and Fourth Assessment Reports (Candela, Elorza, Jiménez-Martínez, & Von Igel, 2012; Stocker et al., 2014).

In the present study, the horizons 2021 and 2027 were considered in hydrological planning as the closest scenarios for the management of resources. Forecasts for global circulation models (75th percentile) for this research area (Mediterranean region) and the less favorable scenarios, RCP4.5 and RCP8.5 estimated by the IPCC, were considered. Data from research nearby where a modeling of resources for future horizons were developed (Jiménez-Fernández & Jiménez-Gavilán, 2014; Jiménez-Gavilán et al., 2015) were also considered (Figure 2).

Figure 2 Maps of temperature and precipitation change for the RCP4.5 scenario (Stocker et al., 2014). 

Uses and demands

To satisfy demands with resources according to the Coordinated Plan extracted from the Hydrological Plan that concerns the supply of water in Malaga, irrigation of the irrigable surface area, and the environmental requirements for the different planned horizons were determined (Table 4).

Table 4 Resources from different uses (hm3). 

Horizon Use Regulated Surface runoff Underground Regenerate Desalinated Total Total
Actual Human supply 34.98 17.24 6.85     59.07 136.31
Irrigated area 59.52 0.69 6.78     66.99
E. Flow           10.25
2021 Human supply 40.43 16.62 7.09     64.14 135.95
Irrigate area 46.65 0.69 6.78     54.12
E. Flow           17.69
2027 Human supply 46.97 14.61 6.24     67.82 139.61
Irrigate area 31.40 0.63 3.39 18.68   54.10
E. Flow           17.69


It is indisputable that agriculture must become sustainable, that is to say, it must meet the needs of present generations without compromising the needs of future generations (WCED, 1987). Sustainability is a multidisciplinary concept that encompasses environmental, social, and economic dimensions. It is necessary to advance sustainability indicators that help the agricultural sector in decisions surrounding productivity, the adoption of a specific technology, or the change of land use. Although scientific interest related to sustainability indicators in agricultural systems is increasing, it is also necessary to make purely economic calculations and then qualify the data with environmental or social aspects.

Drought cycles affect water availability. If the climate change prediction scenarios foreseen by the IPCC for the Mediterranean region are fulfilled, measures directed at limiting irrigation water quantity or investing to make water distribution more efficient to avoid losses.

The Leontief model was used to calculate total economic impact (Leontief, 1986) using the input-output tables available in Andalusia (2010; the last year available). The Leontief demand model is described as:

Y = [I-A] - 1xD

where Y is the total economic impact, [I-A]-1 is the inverse square matrix of regional technical coefficients (it is called the inverse matrix of Leontief), and D is the vector of direct income at basic agricultural prices.

Results and discussion

In the Guadalhorce River valley, and given that the productivity of the irrigable area in the valley is high, the first feasible economic approach was to determine the need for works of irrigation water abstraction and distribution in order to quantify the investments necessary to maintain or expand the irrigable area. According to ICRA data, the research area has an average annual income of 7 613 € ha-1. Of the total irrigable area (12 690 ha), 9 248 ha are irrigated, so the total income from this area amounts to 70 405 024 €. This is a direct impact. The total income from the irrigated area was calculated as 70 405 024 € (Table 5) and was necessary to estimate the D vector.

Table 5 Distribution of direct income. 

Factor Income (€) Percentage (%)
Agriculture, livestock, and fishing 26 385 606.85 37.50
Industry 19 077 085.22 27.10
Construction 9 180 559.89 13.00
Services 15 761 772.03 22.40
Total 70 405 024.00 100.00

The inverse square matrix of regional technical coefficients was applied to the direct income vector. The result provided the distribution of production generated by different economic sectors (Table 6).

Table 6 Distribution of production generated by each economic sector. 

Factor Total production Indirect production
Income (€) (%) Income (€) (%)
Agriculture, livestock and fishing 52 270 184.53 29.00 25 884 577.67 23.50
Industry 50 870 046.32 28.20 31 792 961.09 28.90
Construction 23 417 251.72 13.00 14 236 691.83 12.90
Services 53 973 715.42 29.90 38 211 943.39 34.70
Total 180 531 197.98 100.00 110 126 173.98 100.00

The irrigated area directly accounts for 70 million euros, which translates into 180.5 million of total economic impact. Any land-use change approach should take this economic activity into account since environmental sustainability must go hand in hand with social and economic sustainability. Any change in land use would require calculation and discounting of the impacts of the new use.

The irrigable area consisted of 12 690 ha split between irrigated and non-irrigated areas. Non-irrigated area covered a total of 3 442 ha, while the irrigated area was 9 248 ha (Figure 3).

Figure 3 Maps of irrigable (A) and irrigated areas (B). 

The hydrological planning estimates for the 2021 and 2027 horizons project a decrease in demand for irrigation and an increase in the supply and environmental requirements to fulfill the environmental objectives of the water bodies in the research area. In the 2021 horizon, reduced irrigation demand resulted from improved irrigation efficiency while supply resources and environmental requirements increased. In the 2027 horizon, increased demand for water supplies was partly offset by resource contributions from regenerated water while resources were released from the system to improve water management and to continue meeting the environmental objectives of water bodies located in the research area (i.e., Water bodies are not sentient and therefore cannot have objectives. Humans have objectives for the management of water bodies).

However, according to climate change scenario predictions, data indicating reduced water contributions to some hydrologic systems in the southern region of the Iberian Peninsula (Jiménez-Fernández & Jiménez-Gavilán, 2014) and the increased prevalence of torrential rainfalls, it is possible to reduce contributions to the system by 25%. Together with forecasts of increased demand for urban water supply, water deficits will be generated in the area.


Updating of the irrigated area in the Coordinated Plan requires redefinition because of changes in the region during the more than 40 years since its approval and adoption into the new hydrological planning requirements with full entry into the Water Framework Directive. To compensate for the water resources deficits in this area in the future, new resources will require incorporation into the system. Due to the proximity of the research area to the sea, the best option is to construct a desalination plant in the coastal zone to supply the human population, which will guarantee supply under all potential future scenarios.

Deficits in irrigation water generated in less favorable climate change scenarios will be compensated by an increase in the proportion of regenerated resources together with desalination. Simultaneously, less resource-intensive crop varieties should be studied and adopted to reduce irrigation water demand and improve the efficiency of the system.

Classical economic evaluation methods, such as the one presented above, do not consider environmental and social implications. In order to have a true estimation of water resource and land-use planning governance impacts, environmental and social implications require quantification.


n.a. (March, 28, 1961). Order of March 14, 1961, which approves the Coordinated Plan of Works of the irrigable area through the channels of both banks of the Guadalhorce River (Malaga). Official State Gazette, (74), 4769-4773. Recovered from ]

n.a. (November, 7, 1972). Order of October 27, 1972, approving the Coordinated Reformed Works Plan for the irrigated area of the Guadalhorce (Málaga). Official State Gazette, (267), 19785-19788. Recovered from ]

Candela, L., Elorza, F. J., Jiménez-Martínez, J., & Von Igel, W. (2012). Global change and agricultural management options for groundwater sustainability. Computers and Electronics in Agriculture, 86, 120-130. [ Links ]

European Union. (2000). Directive 2000/60/EC of the European Parliament and the Council establishing a framework for the Community action in the field of water policy (Water Framework Directive). Official Journal L, 327. [ Links ]

ICRA, Consejería Agricultura, Pesca y Medio Ambiente, Junta de Andalucía. (2008). Inventario y caracterización de los regadíos de Andalucía. Distritos Mediterráneos y Atlánticos (ICRA 2008) (CD-ROM). Andalucía, Spain: Junta de Andalucía. [ Links ]

Jiménez-Fernández, P. (2010). Sistema de explotación Guadalhorce. Salinización y cambio climático. Malaga: Spain: University of Malaga. [ Links ]

Jiménez-Fernández, P., & Jiménez-Gavilán, P. (2014). Modelización de los impactos del cambio climático sobre el recurso hídrico en la masa de agua subterránea Sierra de Líbar (060.044), sur de España. Implicaciones socio-ambientales. XII Edición Congreso Nacional de Medio Ambiente-CONAMA2014, Madrid, Spain. [ Links ]

Jiménez-Gavilán, P., Jiménez-Fernández, P., Morales-Calvo, L., & Ruiz-Antúnez, R. (2013). Caracterización hidrogeológica e hidrogeológica de diversas áreas limítrofes con las presas del Guadalhorce (provincia de Málaga). Serie: Hidrogeología y Recursos Hidráulicos (30), 125-134. X Simposio de Hidrogeología. Fernández-Uría, A. (ed.), Instituto Geológico y Minero de España, Madrid. [ Links ]

Jiménez-Gavilán, P., & Jiménez-Fernández, P. (2015). Modelling of last hypothesis of climate change impacts on water resources in Sierra de las Cabras aquifer (Southern Spain). In: Andreu J. et al. (eds.). Drought: Research and science-policy interfacing (pp. 57-64). London, UK: Taylor & Francis Group. [ Links ]

Leontief, W. (1986): Input-output economics. London, UK: Oxford University Press on Demand. [ Links ]

Sánchez-García, D. (2010). Aplicación de la Directiva Marco del Agua 2000/60/CE en la cuenca hidrográfica del río Guadalhorce (Málaga). Caracterización inicial. Malaga, Spain: University of Malaga. [ Links ]

Stocker, T. F., Qin, D., Plattner, G.-K., Tignor, M., Allen, S.K., Boschung, J., Nauels, A., Xia, Y., Bex, V., & Midgley P. M. (eds.). (2014). Climate Change 2014: The physical science basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Report of the Intergovernmental Panel on Climate Change (IPCC). Cambridge, UK, New York, USA: Cambridge University Press. [ Links ]

WCED. (1987). Our common future. World Commission on Environment and Development. London, UK: Oxford University Press. [ Links ]

Received: January 31, 2018; Accepted: March 18, 2018

Correspondence author:,

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