Navigation – Plan du site

AccueilNuméros96/1ArticlesProspective integrated modelling ...

Articles

Prospective integrated modelling of water scarcity risk in western Switzerland: lessons learned and new challenges for water security assessment

Modélisation intégrée prospective du risque de pénurie d'eau en Suisse romande : leçons apprises et nouveaux défis pour l'évaluation de la sécurité hydrique
Marianne Milano et Emmanuel Reynard

Résumés

La sécurité hydrique est un concept émergent, dont l’évaluation et la quantification sont en cours de développement. La quantification du stress hydrique peut être considérée comme une recherche de base pour la sécurité hydrique. Cet article s’appuie sur quatre projets de recherche menés par les auteurs en Suisse occidentale permettant de délivrer cinq messages clés : (i) des scénarios tenant compte à la fois des changements hydro-climatiques et socio-économiques sont nécessaires pour saisir leurs impacts respectifs sur la pénurie d’eau ; (ii) la résolution spatiale et temporelle des modèles intégrés doit être adaptée à la question traitée ; (iii) l’implication des parties prenantes pour coproduire des scénarios de demande en eau future et tester des stratégies d’adaptation permettant de réduire les tensions hydriques est nécessaire afin d’augmenter la plausibilité des situations modélisées ; (iv) les approches hydrologiques empiriques doivent évoluer vers une intégration géographique des territoires, notamment pour mieux appréhender les différents usagers de l’eau, et (v) des recherches interdisciplinaires sont nécessaires pour évaluer les ressources en eau en termes de quantité et de qualité, et pour inclure les processus sociaux et de gouvernance dans les exercices de modélisation. Dans une perspective globale, nous pensons que de tels développements méthodologiques permettraient d’évoluer vers une vision dynamique et prospective de la sécurité hydrique.

Haut de page

Notes de l’auteur

The ICCARE-Vaud project and Calianno’s PhD research were financed by the University of Lausanne and received no other specific grant from funding agencies in the public, commercial, or not-for-profit sectors. The MontanAqua project was supported by the Swiss National Science Foundation [grant 406140-125964]. The LABEAU project was funded by the University of Lausanne, as well as by BlueArk Entremont and the company ALTIS SA.

Texte intégral

The authors are grateful to the federal and cantonal offices, local administrations and associations, for providing the necessary data for these modeling exercises. They would also like to acknowledge the Center for Climate Systems Modeling (C2SM) for providing the CH2011 future climatic scenarios. The authors are also grateful to the stakeholders and farmers of the municipalities of Montana and Bagnes for their involvement in the research projects initiated by the authors. Finally, they acknowledge colleagues at the universities of Bern, Lausanne and Fribourg who participated in the MontanAqua and ICCARE-Vaud projects as well as the members of ALTIS SA who collaborated in the LABEAU project.

Introduction

1From a hydrological perspective, the impacts of climatic and socio-economic changes on water resources have mainly been addressed through the lens of physical water scarcity, which highlights potential shortages but does not account for governance and adaptation processes. Several assessments were global and provided insights into the complex functioning of the hydro-social system (see e.g. Sivapalan et al., 2012; Linton and Budds, 2014; Munia et al., 2016) and helped identify areas where future water resources are most vulnerable to climatic and anthropogenic changes (see e.g. Alcamo et al., 2007; Wada et al., 2011; Wieck and Larson, 2012; Mekonnen and Hoekstra, 2016). However, these studies relied on global political economy and water use scenarios that did not always fit local adaptive strategies, instruments and institutional frameworks (Gourbesville, 2008; Milano et al., 2013). The spatial resolution of such studies and their simplification of socio-economic processes and demographic patterns were unable to grasp the complex socio-hydrological functioning of water systems at regional and local scales (Cook and Bakker, 2012). Regional and local scale studies were subsequently conducted to include the political and technical measures taken to avoid unsustainable exploitation of water resources (Lahmer et al., 2001; Schneider and Homewood, 2013; Schneider et al., 2015). These studies identified drivers likely to undergo local and rapid climatic and anthropogenic changes (see e.g. Fabre et al., 2015; Wang et al., 2016; Malek and Verburg, 2018) and assessed the capacity of local adaptation measures to reduce water scarcity (see e.g. Varela-Ortega et al., 2011; Fabre et al., 2016). These research advances are considered useful to involve and inform decision makers (Fant et al., 2016). They are also in the thematic continuity regarding the appreciation of the emerging concept of water security (Cook and Bakker, 2012).

2This concept emerged in the 1940s but has only come to the forefront of hydrological and social research, and of policy debates in the last two decades (Cook and Bakker, 2012; Garrick and Hall, 2014). It is a broad, conceptual, multi-dimensional framework that entails issues of ecosystem and human health, accounts for water quantity and quality issues, and questions existing water governance frameworks and processes (Grey and Sadoff, 2007; Savenije and van der Zaag, 2008; Bakker, 2012; Pahl Wostl et al., 2013, 2016; Bolognesi and Kluser, 2018). It is understood as a key tool to address the multiple challenges associated with water management in the 21st century (UN Water, 2013). However, it is not a ready-made operational concept that can easily be applied, and multiple and incommensurate definitions exist that are used by both researchers and policy makers (Bakker, 2012; UN Water, 2013). Cook and Bakker (2012) called for narrowing the definition and focusing on issues of relevance in the first instance due to the innovative and interdisciplinary nature of the concept. In that respect, in this paper, it is assessed only from the hydrological perspective. Here, we define water security as “the capacity of a population to safeguard access to adequate quantities of water of acceptable quality for sustaining human and ecosystem health on a watershed basis, and to ensure efficient protection of life and property against water related hazards – floods, landslides, land subsidence and droughts” (UNESCO-IHP, 2012, p. 1). This definition frames the concept to the management of two sets of challenges: extreme events such as floods, droughts and pollution issues, and the allocation of water to competing water users under climate change (Wheater, 2015; Young et al., 2015). Research on water scarcity is viewed as a base research for water security assessment that provides data on resource-demand relationships and a primary way of measuring access to sufficient water (Cook and Bakker, 2012).

3Currently, several indicators are used to evaluate water scarcity (Falkenmark et al., 1989, Shiklomanov, 1991; Sullivan, 2002; Pedro-Monzonís et al., 2015) but indicators that combine water resources, ecosystems and human health, and water governance arrangements are rare (Cook and Bakker, 2012; Bakker, 2012; Octavianti and Staddon, 2021). According to the literature, Lautze and Manthrithilake (2012) and Sun et al. (2016) recently developed the two first indexes to quantify water security in Asia, and Gain et al. (2016) suggested a first multi-criteria analysis framework based on the indicators of Goal 6 of Sustainable Development Goals to quantify water security at global scale. These studies aggregated different indicators and revealed the heterogeneous distribution of water security related to the sensitivity of countries to different physical and socio-economic indicators. The studies provide the first large scale analyses that go beyond water scarcity assessment, offer an initial assessment of the water security concept and suggest preliminary paths for quantifying water security. The authors still call for further studies as they had to rely on raw global data with different spatial details and of different quality, water resources availability is still poorly addressed from a qualitative point of view, the understanding of current institutional and policy regimes is too broad and indicators are weighted without sensitivity analyses or the involvement of stakeholders. Therefore, regarding its assessment, interpretation and index-based quantification, water security is still a concept under development.

4As part of the special issue on “Water researchers in times of global change. What future for territories?”, this paper reflects on the conceptual and methodological evolution of water scarcity assessment based on four research projects undertaken in western Switzerland. Although Switzerland is often described as Europe’s water tower (Viviroli and Weingartner, 2004), the factors that affect the risk of present and future water scarcity in Switzerland are a major concern, as the country already experienced several water shortage episodes in the last decade. The most recent drought events (2003, 2011, 2015, 2018, 2019) were remarkably long and the highest summer temperatures were recorded since the beginning of meteorological measurements in 1864 (ProClim, 2005; Begert et al., 2005; FOEN, 2016; Begert and Frei, 2018; FOEN, 2021). Rivers and some springs dried up during summer (FOEN, 2016; 2017; 2019). For the first time, cantonal authorities (the administrative bodies responsible for water distribution) called for water savings and farmers were allocated irrigation turns (FOEN, 2016). These episodes brought important water management issues to light, like the lack of water allocation priorities, the need to define good irrigation practices, and the need for drought prevention plans (FOEN, 2012a; Kruse and Seidl, 2013). The series of droughts also revealed “a moderate state of social capacities regarding drought risk management” (Kruse and Seidl, 2013, p. 3438). Several studies were launched to grasp the impacts of climate change on water resources and their related impacts on hydropower production (Hänggi and Weingartner, 2012; Gaudard et al., 2013; Barry et al., 2015 among others), the effects of alternative water policies on crop yields and farmers’ income (e.g. Finger and Lehman, 2012; Lehman et al., 2013; Lehman and Finger, 2014) and the impacts of land use or waste water treatment plants on water quality (e.g. Ort et al., 2009; Robinson et al., 2014). Critical situations were identified in Alpine catchments where glacier melt could be reduced, thereby affecting the seasonal availability of water resources and altering water storage, in particular for the production of hydroelectricity (Finger et al., 2012; Gaudard et al., 2014; Lane and Nienow, 2019), but also in pre-Alpine catchments where water needs for irrigation could increase significantly (Vanham et al., 2009; Fuhrer and Jasper, 2012; Fuhrer et al., 2014). Western and southern Switzerland in particular will likely be prone to longer dry spells in summer (Schmidli and Frei, 2005; Scherrer et al., 2016) and more intense low flows due to less snow storage and earlier snow melt (see e.g. Stewart, 2009; Beniston and Stoffel, 2014; Morán-Tejeda et al., 2014; Milano et al., 2015a). Coupled with anthropogenic changes such as population growth, increased irrigation and livestock raising in the lowlands, and the expansion of tourism, rivers in western Switzerland can no longer be considered as reliable water sources (FOEN, 2012b, 2021) and conflicts over water are likely to increase (Fuhrer and Jasper, 2012; Fuhrer et al., 2014; Milano et al., 2015b).

  • 1 MontanAqua (2010-2014), financed by the Swiss National Foundation, and ICCARE-Vaud (2013-2015), fin (...)
  • 2 Quantifier les usages de l’eau en territoire touristique de montagne (2013-2018), PhD thesis financ (...)

5In that respect, two research projects1 were created to develop integrated modeling frameworks and assess the risk of water scarcity in western Switzerland. Although their results regarding the occurrence of current and future water scarcity have already been published (Reynard et al., 2014a; Milano et al., 2015a), this paper builds on these projects and provides new outcomes. In particular, the conceptual and methodological progresses and issues of water scarcity assessments are put forward in this paper. With the advances achieved in two other projects2 that focused on water users and their territorial footprint in western Switzerland (Calianno et al., 2018; Milano and Reynard, 2021), possible dimensions for a holistic approach to water scarcity are discussed together with the appropriate geographical scale to represent the relationships between water resources and water uses.

Case studies

  • 3 The municipalities of Bagnes and Vollèges merged on 1st January 2021 to form the commune of Val de (...)

6The four research projects on which this paper draws focus on western Switzerland, more specifically on nine meso-scale catchments (38–637 km2) of the canton of Vaud (Switzerland), the Crans-Montana-Sierre (CMS) area (130 km2) and the municipality of Bagnes3 (282 km2) in the canton of Valais.

7In the canton of Vaud, catchments extend from the Jura Mountains (alt. max. 1’677m.a.s.l.) over the Swiss Plateau (400–600m.a.s.l) to the high Alpine mountains (alt. max. 3’200m.a.s.l; Fig. 1). Mean annual temperatures range from 10°C to 4°C and mean annual precipitation vary from 865 to 2’020mm/year, from low to high altitudes (average for the 1984–2005 period; Milano et al., 2015b). The shores of Lake Geneva and Lake Neuchâtel are marked by strong urban and peri-urban development. Agricultural activities characterize the plains and piedmont, and account for 17% of Swiss agricultural land (FSO, 2006), while dairy cow breeding dominates in mountainous areas. In this paper, special attention is paid to the Venoge, Talent and Grande Eau catchments that are representative of hydro-climatic and anthropogenic stakes in the Lake Geneva Region, Plateau and Alpine areas of the canton of Vaud, respectively (Table 1).

Figure 1: Geographical location of the (1) Venoge, (2) Talent and (3) Grande Eau catchments, the (4) Crans-Montana-Sierre area and (5) the municipality of Bagnes

Figure 1: Geographical location of the (1) Venoge, (2) Talent and (3) Grande Eau catchments, the (4) Crans-Montana-Sierre area and (5) the municipality of Bagnes

VD – canton of Vaud, VS – canton of Valais. The dashed lines show the borders of the catchments studied in the ICCARE-Vaud project (Milano et al., 2015a,b) but not presented in this paper.

8The Crans-Montana-Sierre (CMS) area is located on the northern rim of the Rhone River valley (Fig. 1). It ranges from 519m.a.s.l in the Rhone River valley to 3’100m.a.s.l in the Bernese Alps mountains, and is partly covered by the Plaine Morte glacier (7.32km2 in 2016; www.glamos.ch). Temperature and precipitation follow a steep vertical gradient (Table 1). The area benefits from a high level of sunshine and dry conditions in summer due to the climate barrier formed by the Swiss Alps. Vineyards thus predominate up to an altitude of about 800m. Above 800m, the CMS area is characterized by forests, grasslands and cattle raising. Higher altitudes (>1’400m.a.s.l) host one of the largest tourist resorts in Switzerland: Crans-Montana offers 40’000 beds and is very attractive for skiing in winter and golf and hiking in summer. Bagnes municipality (282km2) is located on the southern rim of the Rhone River valley (Fig. 1) between 790 and 4’314m.a.s.l. From low to high altitudes, mean annual temperature ranges from 8 to - 5°C and mean annual precipitation from 1’013 to more than 2’000mm, (MeteoSwiss, 2021). Bagnes municipality contains 68.8% of unproductive land (glaciers, lakes, areas with no vegetation or unproductive vegetation) and 0.2% of nature protected area, mainly at high altitudes, 18.6% of agricultural land and 11% of forests at mid-altitude, and 1.5% of urban area in the valley bottoms including the tourist resort of Verbier.

Table 1: Characteristics of the Venoge, Talent and Grande Eau catchments (canton of Vaud), the Crans-Montana-Sierre area and the municipality of Bagnes (canton of Valais)

Canton of Vaud

Canton of Valais

Venoge

Talent

Grande Eau

Crans-Montana-Sierre

Bagnes

Geographical context

Area (km2)

231

62

134

130

282

Range of altitude (m.a.s.l)

382 – 1677

440 – 929

410 – 3’200

519 – 3’100

790 – 4’314

Hydro-climatic context (average over the 1984-2005 period in the Canton of Vaud; 1981-2010 in the CMS area; MeteoSwiss, 2016)

Mean annual temperature (°C)

9.1

9.5

5.0

10.1 to -2.7

8 to -5

(from valleys to mountain crests)

Mean annual precipitation (mm)

1’075

1’175

1’587

672 to >2’500 1013 to >2’000

(from valleys to mountain crests)

Mean runoff (m3/s)

4.1

1.1

4.8

5.3

2.03

Specific runoff (L/s/km2)

17.7

17.7

35.8

40.8

6.9

Land use (2013)

Urban (%)

19

11

7

8

1.5

Forest (%)

2

21

16

28

11

Cropland and grassland (%)

77

68

75

27

18.6

Vineyard (%)

2

0

0

8

0

Other (ice and rock,%)

0

0

1

29

68.8

Material and methods

9The ICCARE-Vaud and MontanAqua projects have been the subject of several scientific papers and reports in which the methods are described in great detail (Milano et al., 2015a, b; Reynard et al., 2014a; Weingartner et al., 2014; Schneider and Rist, 2014; Schneider et al., 2015). Only a summary of the methods is thus presented here. The PhD thesis (Calianno, 2018) and the LABEAU project were conducted in a second phase to extend knowledge on water uses.

An integrated and systemic modeling approach

10In all four projects, hydrosystems were considered as a series of interrelated entities with natural, social and economic features (Chorley and Kennedy, 1971). In particular, an integrated and systemic modeling approach was developed to address interactions between climate, freshwater availability, freshwater withdrawals and water management options in the ICCARE-Vaud and MontanAqua projects (Fig. 2). Daily freshwater availability and water needs were estimated over a past reference period (1984-2005 for the canton of Vaud and 2006-2011 for the CMS area) and by mid-century (2050-2071 for the canton of Vaud and 2037-2041 for the CMS area). Results were aggregated at a monthly time step for synthesis purposes. Past daily meteorological data were collected from the automatic meteorological network of Switzerland and interpolated using the detrended inverse distance weighting method. For prospective modeling, delta change signals extracted from ten regional climate models forced with the IPCC A1B greenhouse gas emission scenario (Bosshard et al., 2011; CH2011, 2011) were applied on daily temperature and precipitation series. For synthesis purposes and key messaging, the median hydro-climatic evolution is presented in this paper. Future water needs were estimated based on a business-as-usual scenario but also, in the CMS region, based on alternative land use scenarios co-constructed during focus groups with local water stakeholders (Schneider and Rist, 2014; Schneider et al., 2015). Finally, water scarcity was quantified based on a water scarcity index, i.e. a ratio of monthly water needs to monthly available freshwater resources (Shiklomanov, 1991). This index expresses the intensity of pressure applied by water needs on available water resources: the higher the index, the greater the scarcity. In all four studies, water resources were evaluated based only on surface waters.

Figure 2: Methodological approach

Figure 2: Methodological approach

In black: methodology core, in grey: additional data for future state assessment. P: Precipitation, T: Temperature

11In support of these integrated modeling research projects, statistical analyses of water volumes measured daily at the outlet of the reservoirs of the drinking water distribution network in the municipalities of Montana and Bagnes were performed between January 2015 and December 2017. In Montana, these analyses were combined with statistical analyses of daily irrigation time series collected using metering devices specifically installed for the project, as well as qualitative interviews with the drinking water department managers five winegrowers and one farmer. The purpose of these additional studies was to improve knowledge and methods related to water use quantification (Fig. 2).

Freshwater evaluation

12In catchments in the canton of Vaud, available freshwater resources were considered as the daily contribution of rapid, delayed and slow runoffs modeled by the semi-distributed and process-oriented PREVAH model (Viviroli et al., 2009). Further information on the model structure, and on the datasets and calibration-validation procedure used can be found in Viviroli et al. (2009) and Milano et al. (2015b), respectively.

13Freshwater supply in CMS relies on the headwaters of the area, composed of springs and the Plaine Morte Glacier. Freshwater resources coming from the headwaters were modeled by the MontanAqua team using the Glacier Evolution Runoff Model (GERM) (Huss et al., 2008) and the hydrological model Penn State Integrated Hydrologic Model (PIHM, Kumar, 2009). Further information on the structure and performance of the model can be found in Huss et al. (2008), Kumar (2009) and Kauzlaric (2015).

Evaluation of water use

  • 4 In the canton of Vaud, hydropower is mainly run-of-river production and is highly regulated by long (...)

14In the canton of Vaud, water needs were considered as the sum of freshwater volumes required by irrigated agriculture, livestock farming and the domestic sector4 and were projected based on a busines-as-usual scenario.

15Irrigation water needs were evaluated according to the crop coefficient approach (Allen et al., 1998). This method defines the volume of freshwater necessary to meet crop evapotranspiration in addition to rainfall, based on climatic data, cropping patterns and crop growth coefficients. These data were provided by the Federal Statistical Office (2013) and the MandaTerre (2013) association at the municipal level. For future projections, irrigated crops and surface areas were assumed to remain unchanged, but the impacts of climate change on crop water needs were explored. Further information on the model dataset and process can be found in Milano et al. (2015b).

16Livestock water needs, i.e. the quantity of water required to water farm animals, were computed for each municipality by multiplying the specific water needs of each livestock species by the number of animals of the species concerned. Specific livestock water needs were defined using different literature sources (Sautier, 2004; Ward and McKague, 2007; Collier and Lillywhite, 2011) and the Federal Statistical Office provided the annual number of animals in each municipality (FSO, 2013). Past livestock trends were continued for future projections.

17Urban water needs, i.e. water needs for households, businesses connected to the communal network and maintenance of the municipalities, were estimated for each municipality by multiplying the national unit per capita water allocation by the population of the municipality (SGWA, 2013; Canton of Vaud, 2013). Annual variations in unit water allocation and population were taken into account. For future estimates, it was assumed that water-saving efforts and progress in hydraulic efficiency would compensate for increasing water needs related to population growth. The 2012-unit water allocation was used in future simulations. The canton of Vaud provided annual population projections (Statistique Vaud, 2011).

  • 5 As this use is strictly regulated by long-term concessions (and therefore does not influence the wa (...)

18In the CMS area, water needs for the irrigation of agricultural plots and golf courses, the urban sector as well as for artificial snowmaking were evaluated from 2006 to 2011. They were estimated based on an intense documentary survey conducted in collaboration with the municipal administrations, technical managers, and the population, combined with the monitoring of several irrigation canals (Bonriposi, 2013). Water used for hydropower production was not included5. For future estimates, four different regional development scenarios were built with the support of a stakeholder group composed of politicians and local representatives of public administrations, associations and private companies (Schneider and Rist, 2014):

  • business-as-usual scenario: the regional development of the CMS area relies on economic growth based on mass tourism and on the expansion of built-up areas. The population continues to increase while agriculture continues to decline. Water issues are assumed to be solved through technical measures.

  • Stabilizing scenario: regional planning is improved by intercommunal collaboration. Four-season tourism is expanded, construction is restricted and agriculture remains a core economic activity. Water management aims to optimize water consumption by regulating water users and improving irrigation techniques.

  • Moderate scenario: “soft” tourism and water saving efforts are promoted. Artificial snowmaking is abandoned and drip irrigation is adopted for vineyards.

  • Shared strategy: this scenario was suggested by the stakeholders. It considers that the economic growth of the area is balanced by social needs (equity between citizens) and ecological considerations. Constructions of second homes is restricted. Four-season tourism is developed with an emphasis on agriculture and vineyards.

19Each scenario was translated into changes in land-use and population growth with the support of the stakeholder group (Bonriposi, 2013). Based on these assumptions, future irrigation and urban water needs were evaluated using the same methods as those used in the canton of Vaud. For artificial snowmaking, the potential snow covered area supported by artificial snowmaking was first defined according to altitude and future air temperature, then multiplied by the unit water allocation for snowmaking (L/m2).

Results

Future changes in water scarcity in western Switzerland

20Currently, the highly irrigated Venoge and Talent catchments experience moderate water scarcity from May to September and severe water scarcity in July and August as total water needs exceed 80% of freshwater available in rivers (Fig. 3a). The Grande Eau pre-Alpine catchment does not suffer from water scarcity (Fig. 3a). The CMS area currently does not suffer from water scarcity in the summer season but is subject to moderate to high water scarcity over the rest of the year. Water scarcity is even defined as severe in the winter months (January–February–March) and in September (Fig. 3a).

21By mid-century, under the business-as-usual scenario, the Venoge and the Talent catchments may experience moderate to high water scarcity in May and September and severe water scarcity from June to August (Fig. 3b). In particular, the needs for water could exceed the freshwater available during these months. The Grande Eau catchment should continue to be spared water scarcity all year round (Fig. 3b). The CMS area could experience high to severe water scarcity from November to March and in August and September (Fig. 3c). However, alternative scenarios could prevent the region from experiencing severe water scarcity in winter as these scenarios could limit total water needs to 50-70% of the available freshwater resources. However, only the moderate scenario would prevent the region experiencing severe water scarcity in late summer, although water scarcity would still remain high. Finally, irrespective of the scenario, the region should not suffer from any water scarcity during the summer season.

Figure 3: Current and future water scarcity in catchments of the canton of Vaud and in the Crans-Montana-Sierre area based on the water scarcity index

Figure 3: Current and future water scarcity in catchments of the canton of Vaud and in the Crans-Montana-Sierre area based on the water scarcity index

Source: Shiklomanov, 1991

Causes of the risk of water scarcity in western Switzerland

Changes in freshwater availability

22Currently, the risk of water scarcity in western Switzerland coincides with low flow. The river Venoge, which is representative of rivers flowing from the Jura Mountains to Lake Geneva, and the Talent, which is representative of rivers on the Swiss Plateau, are characterized by low flows during the summer season due to the end of snowmelt and less precipitation, respectively (Table 2; Fig. 4a). The pre-Alpine catchment Grande Eau and the headwaters of the CMS area are characterized with low flows in winter due to snow and ice accumulation (Table 2; Fig. 4d).

Table 2: Seasonal freshwater availability in four hydrosystems in western Switzerland

Catchment

Area (km2)

Hydrological regime

Seasonal runoff (m3/s)

JFM

AMJ

JAS

OND

Venoge (VD)

231

Nivo-pluvial

15.2

11

4.7

12.4

Talent (VD)

62

Pluvial

4.0

2.5

1.7

3.9

Grande Eau (VD)

134

Nival

8.6

20.8

13.1

9.8

Headwaters of CMS area (VS)

130

Nivo-glacial

0.74

10.6

7.8

2.1

Seasonal runoff is averaged over the 1984-2005 period for the Venoge, Talent and Grande Eau catchments (canton of Vaud – VD) and over the 2006-2011 period for the CMS area (canton of Valais – VS).

23By mid-century, temperatures are expected to rise by 2–3 °C in western Switzerland throughout the year and by a further 1 °C in summer. Precipitation is projected to increase by 10–30% from October to May in the Lake Geneva Region and to decrease by 20–30% in summer over the Plateau and the Alps. In addition, up to 2’000 m a.s.l., rainfall should increase at the expense of snowfall as a result of rising temperatures (data not shown). Changes in the liquid-solid precipitation ratio should lead to less snow accumulation in winter and to a 56% reduction in ice volume in the Plaine Morte glacier (Huss et al., 2013).

  • 6 After 2060, the glacier will be too small to continue having a positive impact on river flows.

24Under climate change, low flows are expected to become more severe in the Venoge and Talent rivers with a 15% decrease in runoff due to less snowmelt in spring and changes in precipitation distribution (Fig. 4a and 4b). In Alpine catchments, river flows should increase from October to February (+20% in the Grande Eau; Fig. 4) and decrease from March to September (-30%) due to changes in snow accumulation. Yet the higher ice melt related to the glacier retreat could offset changes in the liquid-solid precipitation ratio (Huss et al., 2013), maintaining river flows near their current level all year round (± 10% in the CMS area; Fig. 4d)6.

Figure 4: Changing trends in water resources in western Switzerland

Figure 4: Changing trends in water resources in western Switzerland

25Current availability of freshwater resources and water needs and future changes under climate change by mid-century in the (a) Venoge, (b) Talent and (c) Grande Eau catchments, and (d) in the CMS area. Results are based on ten regional climate models but for the purpose of readability and key messaging, median water resources availability and needs are presented here.

Future changes in water needs in western Switzerland

26Currently, total water needs are highest in the Venoge and Talent catchments (21.7Hm3/year and 12.3Hm3/year, respectively) due to high irrigation water needs that amount to nearly three-quarters of the total water needs (Fig. 4a and b). In the Grande Eau catchment, total water needs are low (3.6Hm3/year). Finally, in the CMS area, total water needs amount to 10.9Hm3/year. Its domestic sector uses the most water (59%) followed by the irrigation of agricultural plots and golf courses (37.7%) and artificial snowmaking (3.3%; Fig. 4d). In all four study areas, water needs are constant between October and March, and start increasing in April when irrigation practices begin (Fig. 4). Production of snow in the CMS area is seasonal and occurs between November and February.

27By mid-century and under a business-as-usual scenario, total water needs are expected to increase by 10-20% in the Venoge and Talent catchments (Fig. 4a and b). Annual urban water needs are expected to increase by 40% and livestock water needs to quadruple - although water needs would remain low in this sector compared to other sectors (0.1Hm3/year) - and irrigation water needs are expected to remain high. In the Grande Eau catchment, total water needs are expected to increase by 35% mainly due to a 35-40% increase in urban and agricultural water needs (Fig. 4c). In the CMS area, under the business-as-usual scenario, total water needs are expected to increase by 24% due to an increase in water needs by the domestic sector (+35%), for golf course irrigation (+8%) and for artificial snow making (+77%; Fig. 4d). However, the reduction in the agricultural surface area could lead to a 15-20% decrease in the need for irrigation water.

28Under a stabilizing scenario, however, total water needs could increase by 19% in the CMS area due to a 10-25% increase in urban and irrigation water needs and a 19% decrease in artificial snowmaking, owing to a decrease in the area and length of the periods of artificial snowmaking (Fig. 4d). On the other hand, if water saving efforts were made by domestic users, irrigation practices were improved, and artificial snowmaking were abandoned, as assumed in the moderate scenario, total water needs could decrease by 13%. Finally, total water needs could remain at their current level if the development of the CMS area is balanced. Changes assumed under the shared scenario would increase urban water needs (+8%) and irrigation of golf courses (+6%) but reduce artificial snowmaking (-19%).

Assessing water demand

29The monitoring of water uses in the municipalities of Montana and Bagnes over several years highlighted water consumption patterns and seasonal differences. The biggest seasonal changes in water use are found in the tourist resorts of Montana and Verbier, as well as in hotels and secondary homes. The most significant peaks occur during the end-of-year holidays, the February winter holidays and between mid-July and mid-August. Very intense peaks in water distribution to main homes are related to abrupt activation of spas and/or watering the garden. In Montana, watering gardens can account for as much as 40% of domestic water use between June and August. Calianno et al. (2018) thus suggest defining water use regimes that mirror hydrological regimes. Based on this concept, the seasonal water use regime of the two mountain tourist resorts studied here includes two high seasons (winter and summer) and two low seasons (spring and fall).

30We also compared the irrigation water needs simulated by the CROPWAT agronomic model with data resulting from monitoring conducted in the municipality of Montana (Calianno, 2018). The model tends to overestimate actual water use because it simulates the optimal amount of water needed by the crop, which does not correspond to the quantities actually delivered to the plants by the irrigators. Simulated water needs were 10 to 19 times higher than measured irrigation amounts (Calianno, 2018). These results underline the importance of analyzing irrigation practices to be sure the model parameters match the real practices.

Discussion

Dimensions to be taken into account when assessing water scarcity

31This paper is based on the assessment of water scarcity in several catchments in western Switzerland characterized by different hydrological regimes and seasonal water users and trends. Like previous regional studies, it underlines the fact that such assessments are useful to identify the areas and seasons most prone to water scarcity and to address the capacity of adaptation strategies to reduce the risk. In western Switzerland, the period most vulnerable to water scarcity is during low flows: either in summer in the Lake Geneva and Plateau regions (and in Alpine regions by mid-century) due to high irrigation and urban water needs, or in winter in Alpine areas due to urban water needs during the tourist high season and artificial snowmaking.

32Based on these analyses, four main conclusions can be drawn regarding water scarcity assessment. The first is the need to consider both hydro-climatic and anthropogenic factors when exploring possible future changes in water systems. In catchments in the canton of Vaud, population growth, irrigation practices and changes in livestock rearing practices should increase both water needs and pressure on water resources, while climate change should lead to longer and more intense low flow periods, reducing available water resources when water needs are highest. Water scarcity could continue over a longer period of time by mid-century. In the CMS area, freshwater resources should remain near their current level at mid-century, mainly thanks to the contribution of glacier melt to summer runoff. Water scarcity would then be caused by changing water needs and the degree of the severity would depend on water management options. Climatic and anthropogenic changes have cumulative effects that must be taken into account when exploring possible water management plans.

33A second conclusion is the need for an appropriate time scale to guarantee the risks of water scarcity are properly understood and to build realistic socio-economic scenarios. Most regional studies explore water scarcity on an annual basis (e.g. Menzel and Matovell, 2010; Buytaert and De Bièvre, 2012; Klug et al., 2012; Milano et al., 2013), thereby masking intra-annual temporal variations. For example, the CMS area does not experience any water scarcity on an annual basis but our monthly analysis showed that conflicts concerning water could arise during the winter season and are expected to arise in late summer by mid-century. Seasonal or monthly analysis of water scarcity hence help identify the length of water scarcity episodes, i.e. periods when conflicts are most likely to occur. This issue was also covered by Mekkonnen and Hoekstra (2016) at the global scale. These authors reported that 3.97 billion people currently experience severe water scarcity for at least one month per year, whereas when they used an annual approach, they only identified 2.7 billion people. They argue that studies carried out on an annual basis thus underestimate water scarcity and the number of people affected. Building scenarios with stakeholders also underlines the importance of the choice of time scale. Water shortage in the CMS area is most likely to happen by the end of the century due to the complete melting of the Plaine Morte glacier by 2080 (data not shown, Huss et al., 2013; Kauzlaric, 2015). However, it was difficult for the stakeholders to build realistic regional development scenarios after 2050 due to the speed of territorial changes and the uncertainties of economic development (Reynard et al., 2014b). Water scarcity assessment should thus focus on potential short or medium term changes.

34A third conclusion concerns the spatial scale. Specific studies of water demands in the municipalities of Montana and Bagnes revealed different water use dynamics and typologies between sectors and types of housings. It thus seems necessary to stop assessing water demand at the regional (Saulnier et al., 2011; Coll et al., 2015), catchment (Milano et al., 2013; Fabre et al., 2015), municipal (Bonriposi, 2013; Leroy, 2015; Calianno, 2018) or matrix scale (Vanham et al., 2011), and to move towards the assessment of water use basins. This concept, which was suggested by Calianno et al. (2018), aims to map the spatial footprint of water users and describe the spatial distribution of water demands within a municipality or region. Adding the concept of water use regime would make it possible to characterize the temporal intra-annual distribution of water demands. The combination of water resources and water demand and their spatial and temporal distribution targets high-resolution computing of water scarcity and the identification of water scarcity hot spots, i.e. places and periods with high water stress. We believe that such an approach will support dynamic water demand management, and hence facilitate planning of storage infrastructure.

35A fourth conclusion is the added value of working with local stakeholders and water managers. The assessment and modeling of future water needs and potential stress will be dynamic as long as anthropogenic changes and adaptation measures are taken into account. To give an example, in the canton of Vaud, water needs were only explored using a business-as-usual scenario even though water use practices are highly likely to change (e.g. through the expansion of drip irrigation). In addition, water managers in the canton of Vaud expressed interest in expanding their water supply, e.g. by pumping water from Lake Geneva in the case of a water shortage (General Directorate for the Environment of the canton of Vaud, personal communication, May 13th, 2015). Changing one or more of these variables would have a direct impact on future water scarcity. Based on the experience of the MontanAqua project, building alternative water use scenarios with local stakeholders makes it possible to explore water management strategies that are likely as well as their capacity to reduce conflicts over water. Several authors have highlighted the benefits in involving stakeholders (Carr et al., 2012; Fabre et al., 2016; Gain and Giupponi, 2015; Stanghellini and Collentine, 2008; among others). It is an opportunity for researchers to learn more about water management and policy as well as any environmental problems the study area is facing and to understand the drivers of some water needs (e.g. irrigation practices; Calianno, 2018). It is also an opportunity for stakeholders to listen to different opinions and share ideas or information in a structured and organized framework (Schneider et al., 2015). We agree with Wheater (2015, p. 27), who states “stakeholder engagement is a necessity, not an option”. We also believe that stakeholder engagement better guarantees the implementation of scientific results.

Reducing uncertainties and moving from water scarcity to water security

36Water scarcity assessments rely on hydro-climatic and socio-economic data and tools that have their own assumptions and uncertainties and consequently affect the results. The aim of this paper is not to weigh their influence on the results but to highlight the methodological progress that is still required. We would like to underline two types of uncertainty: hydro-climatic uncertainty linked to the lack of knowledge about future change, and methodological uncertainty linked to the difficulty of assessing the needs of different water users.

37The best handled uncertainties are certainly those related to hydro-climatic scenarios. On one hand, several climate models are often used to present a range of possible trends and signals. In this study, 10 RCMs were considered but we decided to present a median result for synthesis purposes. On the other hand, we selected hydrological models with high efficiency values to describe seasonal dynamics and the volumes of runoff (Kauzlaric, 2015; Milano et al., 2015b). Uncertainties mainly arise from only focusing on the quantity of water, likely missing water quality-related concerns. Indeed, freshwater resources may be of poor quality, and consequently be unavailable for water users, which can also lead to water scarcity. In agreement with van Vliet et al. (2017), Vanham et al. (2018) and Octavianti and Staddon (2021) , we argue that water scarcity assessments should now focus on the availability of freshwater resources of acceptable quantity and quality for users in each sector. To our knowledge, two main approaches are currently under development. One relies on the blue, green and grey water footprint concept (Liu et al., 2016). It aims to account for actual water consumption, control water pollution and maintain environmental flows for good ecological habitat conditions. However, the final index is composed of three components rather than a single value, which requires mastery of the water footprint concept to apply the method and interpret the results (Zeng et al., 2013; Liu et al., 2016). The other method adds to the water scarcity index (Shiklomanov, 1991) the extra amount of water necessary to dilute a pollutant and to reach its legal threshold (e.g. water temperature, salinity; van Vliet et al., 2017; Jones and van Vliet et al., 2018). This is a step forward in water scarcity assessment but still requires considering multiple parameters simultaneously. The availability of data is a further challenge to incorporating water quality in water scarcity assessments. Data on water quality vary among regions, even within the same country, and often has a broader time-step than runoff series (Liu et al., 2017).

38Further uncertainties concern the estimation of water needs, which are often higher than actual water demand, because they are based on generic assumptions and often lacks a comprehensive knowledge of their spatial and temporal dynamics (Wada et al., 2011; Grouillet et al., 2015). This is mainly due to scarce data series on water demands recorded with high temporal resolution due to a lack of local monitoring strategy (Calianno, 2018; Calianno et al., 2018). Most assessments regularly use estimations or proxy data, which has two downsides: (1) monthly variations related to seasonal changes (e.g. due to tourism) are hidden, and (2) the growth stage and local discrepancies are not emphasized. The use of agronomic models also tends to overestimate water needs (Calianno, 2018). It is thus urgent to progress from these conventional econometric methods to dynamic models that couple quantitative and qualitative data (House-Peters and Chang, 2011; Qi and Chang, 2011; Rinaudo, 2015). This entails analyzing individual and social behaviors to identify water use practices or regimes (Calianno et al., 2018) and to identify feedback between key variables in the system (Candelieri and Archetti, 2014; Grouillet et al., 2015; Makki et al., 2015). In this way, the identification and spatial and temporal assessment of the economic, social and environmental factors that influence water uses is improved and can support the development of prospective water demand models (Schleich and Hillenbrand, 2009; House-Peters and Chang, 2011; Gössling et al., 2012; Romano et al., 2014).

39In addition to the aforementioned methodological progresses, the hydrological perspective of water scarcity ignores the social values and institutional context of water management (Buchs and Milano, 2014; Wheater, 2015; Gain et al., 2016). Research on water security needs to be more holistic, in particular by integrating the ecological dimension of water, and putting more emphasis on governance issues. This calls for interdisciplinary research to address both hydrological and social water management challenges (Wheater, 2015; Gain et al., 2016; Octavianti and Staddon, 2021). Indeed, water security must be considered as a holistic framework that accounts for five main dimensions (Grey and Sadoff, 2007; Savenije and van der Zaag, 2008; Lautze and Manthrithilake, 2012; Bakker, 2012; Pahl-Wostl et al., 2013, 2016): (i) environmental health – the spatial and temporal availability of water resources in terms of both quantity (including hydraulic disturbances) and quality, as well as measures taken to restore rivers and protect aquatic ecosystems, (ii) the human dimension – the spatial and temporal variability of water users and environmental standards, their needs and their effects on the quantitative and qualitative availability of water resources, (iii) the physical and natural infrastructure – the ability of water users to have sustainable access to water, sanitation and hygiene networks and services, (iv) the economic environment – the productive use of water to sustain economic growth in the food production, industry, and energy sectors of the economy, (v) the social and institutional environment – the institutional framework and policy-making process and the capacity of societies to build resilient communities that can adapt to change and to reduce the risk of natural disasters.

Conclusion

40This paper builds on several research projects conducted to assess water scarcity and water needs in western Switzerland. It emphasizes, on the one hand, the fact that the most vulnerable period to water scarcity in western Switzerland is during low flows, i.e. in summer in the Lake Geneva and Plateau regions and in winter in Alpine areas. On the other hand, it defines the requirements for and challenges to future research on water scarcity, and from a broader perspective, the integration of water scarcity in the water security concept. Integrated hydrological studies on water scarcity currently correctly integrate hydro-climatic and socio-economic changes and test the capacity of plausible adaptation strategies to reduce conflicts over water with the support of stakeholder involvement. However, two main challenges remain: (1) hydrological approaches must better integrate the geographical dimension of territories, in particular to better grasp the different spatial and temporal dynamics and typologies of water users, and (2) interdisciplinary research is required to assess water resources in terms of both quantity and quality, and to include social and governance processes in modeling exercises, in order to provide a comprehensive and easy-to-use water security index.

Haut de page

Bibliographie

ALCAMO J., FLÖRKE M., MÄRKER M., 2007, Future long-term changes in global water resources driven by socio-economic and climatic changes, Hydrological Sciences Journal, vol. 52, p. 247–275. https://doi.org/10.1623/hysj.52.2.247

ALLEN R.G., PEREIRA L.S., RAES D., SMITH M., 1998, Crop evapotranspiration – guidelines for computing crop water requirements, FAO Irrigation and drainage paper 56, 300p.

BAKKER K., 2012, Water security: research challenges and opportunities, Science, vol. 337, n° 6097, p. 914–915. https://doi.org/10.1126/science.1226337

BARRY M., BAUR P., GAUDARD L., GIULIANI G., HEDIGER W., ROMERIO F., SCHILLINGER M., SCHUMANN R., VOEGELI G., WEIGT H., 2015, The future of Swiss hydropower - A review on drivers and uncertainties, SSRN Electronic Journal. https://doi.org/10.2139/ssrn.2663879

BEGERT M., SCHLEGEL T., KIRCHHOFER W., 2005, Homogeneous temperature and precipitation series of Switzerland from 1864 to 2000, International Journal of Climatology, vol. 25, n° 1, p. 6580. https://doi.org/10.1002/joc.1118

BEGERT M., FREI C., 2018, Long-term area-mean temperature for Switzerland – Combining homogenized station data and high resolution grid data, International Journal of Climatology, vol. 38, p. 2792–2807. https://doi.org/10.1002/joc.5460

BENISTON M., STOFFEL M., 2014, Assessing the impacts of climatic change on mountain water resources, Science of the Total Environment, vol. 493, p. 1129–1137. http://dx.doi.org/10.1016/j.scitotenv.2013.11.122

BOLOGNESI T., KLUSER S., 2018, Water security as a normative goal or as a structural principle for water governance, in BRÉTHAUT C. & SCHWEIZER R. (Eds.), A Critical Approach to International Water Management Trends (p. 201–231), Palgrave Macmillan UK. https://doi.org/10.1057/978-1-137-60086-8_9

BONRIPOSI M., 2013, Analyse systémique et prospective des usages de l'eau dans la région de Crans-Montana-Sierre (Suisse), PhD thesis, University of Lausanne, Lausanne, Switzerland. (in French)

BOSSHARD T., KOTLARSKI T., EWEN T., SCHÄR C., 2011, Spectral representation of the annual cycle in the climate change signal, Hydrology and Earth System Sciences, vol. 15, p. 2777–2788. https://doi.org/10.5194/hess-15-2777-2011

BUCHS A., MILANO M., 2014, Regards croisés sur la notion de pénurie d'eau en Espagne : vers un rapprochement interdisciplinaire, Aqueduc.info, vol. 100, p. 13–18. (in French)

BUYTAERT W., DE BIÈVRE B., 2012, Water for cities: the impacts of climate change and demographic growth in the tropical Andes, Water Resources Research, vol. 48, W08503. https://doi.org/10.1029/2011WR011755 (13 p.).

CALIANNO M., 2018, Quantifier les usages de l’eau en territoire touristique de montagne, PhD thesis, University of Lausanne, Lausanne, Switzerland. (in French)

CALIANNO M., MILANO M., REYNARD E., 2018, Monitoring water use regimes and density in a tourist mountain territory, Water Resources Management, vol. 32(8), p. 2783–2799. https://doi.org/10.1007/s11269-018-1958-9

CANDELIERI A., ARCHETTI F., 2014, Identifying typical urban water demand patterns for a reliable short-term forecasting – the icewater project approach, Procedia Engineering, vol. 89, p. 1004–1012. https://doi.org/10.1016/j.proeng.2014.11.218

CANTON OF VAUD, 2013, Organization of water distribution in the canton of Vaud. Maps and tables on active drinking water suppliers by district and communes (state in February 2013). http://www.vd.ch/themes/environnement/eaux/eau-potable/carte-desdistributeurs/ (Accessed March 2015; in French).

CARR G., BLÖSCHL G., LOUCKS D.P., 2012, Evaluating participation in water resource management: A review, Water Resources Research, vol. 48, n° 11, p. 747-762. https://doi.org/10.1029/2011WR011662

CHORLEY R.J., KENNEDY B.A., 1971, Physical geography. A systems approach, London, Prentice-Hall International. 391 p.

CH2011, 2011, Swiss Climate Change Scenarios CH2011. C2SM, MeteoSwiss, ETH, NCCR Climate and OcCC, Zurich. 88 p.

COLLET L., RUELLAND D., BORRELL-ESTUPINA V., DEZETTER A., SERVAT E., 2015, Water supply sustainability and adaptation strategies under anthropogenic and climatic changes of a mesoscale Mediterranean catchment, Science of the Total Environment, vol. 536, p. 589–602. https://doi.org/10.1016/j.scitotenv.2015.07.093

COLLIER R., LILLYWHITE R., 2011, Final report on livestock (University ofWarwick). Identification and knowledge transfer of novel and emerging technology with the potential to improve water use efficiency within English and Welsh agriculture, Defra Project WU0123, 14p. http://www2.warwick.ac.uk/fac/sci/lifesci/wcc/research/resources/wateruse/technology/ (Accessed 11.2019).

COOK C., BAKKER K., 2012, Water security: debating an emerging paradigm, Global Environmental Change, vol. 22, n° 1, p. 94‑102. https://doi.org/10.1016/j.gloenvcha.2011.10.011

FABRE J., RUELLAND D., DEZETTER A., GROUILLET B., 2015, Simulating past changes in the balance between water demand and availability and assessing their main drivers at the river basin scale, Hydrology and Earth System Sciences, vol. 19, n° 3, p. 1263–1285. https://doi.org/10.5194/hess-19-1263-2015

FABRE J., RUELLAND D., DEZETTER A., GROUILLET B., 2016, Sustainability of water uses in managed hydrosystems: human- and climate-induced changes for the mid-21st century, Hydrology and Earth System Sciences, vol. 20, n° 8, p. 3129–3147. https://doi.org/10.5194/hess-20-3129-2016

FALKENMARK M., LUNDQVIST J., WIDSTRAND C., 1989, Macro-scale water scarcity requires micro-scale approaches. Natural Resources Forum, p. 258-267.

FANT C., SCHLOSSER C. A., GAO X., STRZEPEK K., REILLY J., 2016, Projections of water stress based on an ensemble of socioeconomic growth and climate change scenarios: a case study in Asia, PLOS ONE, vol. 11, n° 3, e0150633. https://doi.org/10.1371/journal.pone.0150633

FINGER R., LEHMANN N., 2012, Policy reforms to promote efficient and sustainable water use in Swiss agriculture, Water Policy, vol. 14, n° 5, p. 887–901. https://doi.org/10.2166/wp.2012.152

FINGER D., HEINRICH G., GOBIET A., BAUDER A., 2012, Projections of future water resources and their uncertainty in a glacierized catchment in the Swiss Alps and the subsequent effects on hydropower production during the 21st century, Water Resources Research, vol. 48, n° 2. https://doi.org/10.1029/2011WR010733

FOEN – FEDERAL OFFICE FOR THE ENVIRONMENT, 2012a, Gérer les pénuries locales d’eau en Suisse, Rapport du Conseil fédéral en réponse au postulat “Eau et agriculture. Les défis de demain”, Office fédéral de l’environnement, Division Eaux, Berne. 88 p. (in French)

FOEN, 2012b, Impacts des changements climatiques sur les eaux et les ressources en eau. Rapport de synthèse du projet « Changement climatique et hydrologie en Suisse » (CCHydro), Office fédéral de l’environnement, Berne, Connaissance de l’environnement, n° 1217, 76 p. (in French)

FOEN, 2016, La canicule et la sécheresse de l'été 2015 : impacts sur l’homme et l'environnement, Office fédéral de l’environnement, Berne, État de l’environnement, n° UZ-1629, 108 p. (in French)

FOEN, 2017, Impulsions pour une adaptation de la Suisse aux changements climatiques. Conclusions de 31 projets pilotes sur l’adaptation aux changements climatiques, Office fédéral de l’environnement, Berne. Info Environnement, n° 1703, 96 p. (in French)

FOEN, 2019, La canicule et la sécheresse de l’été 2018, Office fédéral de l’environnement, Berne, État de l’environnement, n° UZ-1909-F, 91 p. (in French)

FOEN, 2021, (ed.) Effects of climate change on Swiss water bodies. Hydrology, water ecology and water management. Bern, Federal Office for the Environment FOEN, Bern, Environmental Studies, n° 2101, 125 p.

FUHRER J., JASPER K., 2012, Demand and supply of water for agriculture: influence of topography and climate in pre-alpine, mesoscale catchments, Natural Resources, vol. 03, n° 03, p. 145–155. https://doi.org/10.4236/nr.2012.33019

FUHRER J., SMITH P., GOBIET A., 2014, Implications of climate change scenarios for agriculture in alpine regions — A case study in the Swiss Rhone catchment, Science of the Total Environment, vol. 493, p. 1232–1241. https://doi.org/10.1016/j.scitotenv.2013.06.038

FSO – FEDERAL STATISTICAL OFFICE, 2006, Agriculture in the Swiss cantons. Results from the regional accounts of 2005, FSO, Neuchâtel. 34 p. (in French).

FSO, 2013, Farming businesses, utilized agricultural areas and animals from 1975 to 2013 at the cantonal and commune level. www.bfs.admin.ch (Accessed 11.2019).

GAIN A. K., GIUPPONI C., 2015, A dynamic assessment of water scarcity risk in the Lower Brahmaputra River Basin: An integrated approach, Ecol. Indicat. 48, 120–131. https://doi.org/10.1016/j.ecolind.2014.07.034

GAIN A. K., GIUPPONI C., WADA Y., 2016, Measuring global water security towards sustainable development goals, Environmental Research Letters, vol. 11, n° 12, 124015. https://doi.org/10.1088/1748-9326/11/12/124015

GARRICK D., HALL J.W., 2014, Water security and society: Risks, metrics, and pathways, Annual Review of Environment and Resources, vol. 39, p. 611–639. https://doi.org/10.1146/annurev-environ-013012-093817

GAUDARD L., GILLI M., ROMERIO F., 2013, Climate change impacts on hydropower management, Water Resources Management, vol. 27, n° 15, p. 5143–5156. https://doi.org/10.1007/s11269-013-0458-1

GAUDARD L., ROMERIO F., DALLA VALLE F., GORRET R., MARAN S., RAVAZZANI G., STOFFELM., VOLONTERIO M., 2014, Climate change impacts on hydropower in the Swiss and Italian Alps, Science of the Total Environment, vol. 493, p. 1211–1221. https://doi.org/10.1016/j.scitotenv.2013.10.012

GÖSSLING S., PEETERS P., HALL C.M., CERON J.-P., DUBOIS G., LEHMANN L.V., SCOTT D., 2012, Tourism and water use: Supply, demand, and security. An international review, Tourism Management, vol. 33, n° 1, p. 1-15. https://doi.org/10.1016/j.tourman.2011.03.015

GOURBESVILLE P., 2008, Challenges for integrated water resources management. Physics and Chemistry of the Earth, Parts A/B/C, vol. 33, n° 5, p. 284–289. https://doi.org/10.1016/j.pce.2008,02.002

GREY D., SADOFF C. W., 2007, Sink or Swim? Water security for growth and development, Water Policy, vol. 9, n° 6, p. 545–571. https://doi.org/10.2166/wp.2007,021

GROUILLET B., FABRE J., RUELLAND D., DEZETTER A., 2015, Historical reconstruction and 2050 projections of water demand under anthropogenic and climate changes in two contrasted Mediterranean catchments, Journal of Hydrology, vol. 522, p. 684–696. http://dx.doi.org/10.1016/j.jhydrol.2015.01.029.

HÄNGGI P., WEINGARTNER R., 2012, Variations in discharge volumes for hydropower generation in Switzerland, Water Resources Management, vol. 26, n° 5, p. 1231–1252. https://doi.org/10.1007/s11269-011-9956-1

HOUSE-PETERSL A., CHANG H., 2011, Urban water demand modeling: Review of concepts, methods, and organizing principles, Water Resources Research, vol. 47, W05401. https://doi.org/10.1029/2010WR009624

HUSS M., FARINOTTI D., BAUDER A., FUNK M., 2008, Modelling runoff from highly glacierized alpine drainage basins in a changing climate, Hydrological Processes, vol. 22, p. 3888–3902. https://doi.org/10.1002/hyp.7055

HUSS M., VOINESCO A., HOELZLE M., 2013, Implications of climate change on Glacier de la Plaine Morte, Switzerland. Geographica Helvetica, vol. 68, n° 4, p. 227–237. https://doi.org/10.5194/gh-68-227-2013

JONES E., VAN VLIET M., 2018, Drought impacts on river salinity in the southern US: Implications for water scarcity, Science of the Total Environment, vol. 644, p. 844–853. https://doi.org/10.1016/j.scitotenv.2018.06.373

KAUZLARIC M., 2015, A physically based hydrological framework to assess the effects of climate change in a data sparse alpine environment, PhD thesis, University of Bern, Bern, Switzerland.

KLUG H., DABIRI Z., HOCHWIMMER B., ZALAVARI P., 2012, Assessing drinking water consumption by inhabitants and tourists in the Alps using a WebGIS for information distribution, International Journal of Biodiversity Science, Ecosystem Services and Management, vol. 8, n° 1–2, p. 50–70. http://dx.doi.org/10.1080/21513732.2012.680499

KRUSE S., SEIDL I., 2013, Social capacities for drought risk management in Switzerland. Natural Hazards and Earth System Sciences, vol. 13, n° 12, p. 3429–3441. https://doi.org/10.5194/nhess-13-3429-2013

KUMAR M., 2009, Toward a hydrologic modeling system, PhD Thesis, Pennsylvania State University, Department of Civil and Environmental Engineering.

LAHMER W., PFÜTZNER B., BECKER A., 2001, Assessment of land use and climate change impacts on the mesoscale, Physics and Chemistry of the Earth, vol. 26, n° 7–8, p. 565–575. https://doi.org/10.1016/S1464-1909(01)00051-X

LANE S.N., NIENOW P.W., 2019, Decadal-scale climate forcing of alpine glacial hydrological systems, Water Resources Research, vol. 55, p. 2478-2492. https://doi.org/10.1029/2018WR024206

LAUTZE J., MANTHRITHILAKE H., 2012, Water security: Old concepts, new package, what value? Natural Resources Forum, vol. 36, p. 76–87. https://doi.org/10.1111/j.1477-8947.2012.01448.x

LEHMANN N., FINGER R., KLEIN T., CALANCA P., WALTER A., 2013, Adapting crop management practices to climate change: Modeling optimal solutions at the field scale, Agricultural Systems, vol. 117, p. 55–65. https://doi.org/10.1016/j.agsy.2012.12.011

LEHMANN N., FINGER R., 2014, Economic and environmental assessment of irrigation water policies: A bioeconomic simulation study, Environmental Modelling & Software, vol. 51, p. 112–122. https://doi.org/10.1016/j.envsoft.2013.09.011

LEROY E., 2015, Proposition d’interface Science-Société pour la gestion intégrée de la ressource en eau dans un contexte de changements climatiques, PhD thesis, Université de Grenoble. (in French)

LINTON J., BUDDS J., 2014, The hydrosocial cycle: Defining and mobilizing a relational-dialectical approach to water, Geoforum 57, 170–180. https://doi.org/10.1016/j.geoforum.2013.10.008

LIU J., LIU Q., YANG H., 2016, Assessing water scarcity by simultaneously considering environmental flow requirements, water quantity, and water quality, Ecological Indicators, vol. 60, p. 434–441. https://doi.org/10.1016/j.ecolind.2015.07.019

LIU J., YANG H., GOSLING S. N., KUMMU M., FLÖRKE M., PFISTER S., HANASAKI N., WADA Y., ZHANG X., ZHENG C., ALCAMO J., OKI T., 2017, Water scarcity assessments in the past, present, and future, Earth’s Future, vol. 5, n° 6, p. 545–559. https://doi.org/10.1002/2016EF000518

MAKKI A., STEWART R., BEAL C., PANUWATWANICH K., 2015, Novel bottom-up urban water demand forecasting model: Revealing the determinants, drivers and predictors of residential indoor end-use consumption, Resources, Conservation & Recycling, vol. 95, p. 15–37. https://doi.org/10.1016/j.resconrec.2014.11.009

MALEK Ž., VERBURG P., 2018, Adaptation of land management in the Mediterranean under scenarios of irrigation water use and availability, Mitigation and Adaptation Strategies for Global Change, vol. 23, n° 6, p. 821–837. https://doi.org/10.1007/s11027-017-9761-0

MANDATERRE, 2013, Diagnosis of irrigation water needs in the Vaud canton, Report established for the “Service du développement territorial du canton de Vaud” 42 p. (in French).

MEKONNEN M., HOEKSTRA A., 2016, Four billion people facing severe water scarcity, Science Advances, vol. 2, n° 2, e1500323. https://doi.org/10.1126/sciadv.1500323

MENZEL L., MATOVELLE A., 2009, Current state and future development of blue water availability and blue water demand: a view at seven case studies, Journal of Hydrology, vol. 384, p. 245–263. http://dx.doi.org/10.1016/j.jhydrol.2010.02.018.

METEOSWISS, 2021, Climate diagrams and normals per station. https://www.meteoswiss.admin.ch/home/climate/swiss-climate-in-detail/climate-normals/climate-diagrams-and-normals--per-station.html (last accessed June 2021).

MILANO M., RUELLAND D., FERNANDEZ S., DEZETTER A., FABRE J., SERVAT E., FRITSH J-M., ARDOIN-BARDIN S., THIVET G., 2013, Current state of Mediterranean water resources and future trends under climatic and anthropogenic changes, Hydrological Sciences Journal, vol. 58, n° 3, p. 498–518. https://doi.org/10.1080/02626667.2013.774458

MILANO M., REYNARD E., KÖPLIN N., WEINGARTNER R., 2015a. Climatic and anthropogenic changes in Western Switzerland: Impacts on water stress, Science of the Total Environment, vol. 536, p. 12–24. https://doi.org/10.1016/j.scitotenv.2015.07.049

MILANO M., REYNARD E., BOSSHARD N., WEINGARTNER R., 2015b. Simulating future trends in hydrological regimes in Western Switzerland, Journal of Hydrology: Regional Studies, vol. 4, p. 748–761. https://doi.org/10.1016/j.ejrh.2015.10.010

MILANO M., REYNARD E., 2021, LABEAU : Mise en place d’un observatoire des usages de l’eau à l’échelle régionale. Etude préliminaire sur l’approvisionnement en eau potable dans la commune de Bagnes, Université de Lausanne, 33 p.

MORÁN-TEJEDA E., LORENZO-LACRUZ J., LÓPEZ-MORENO J.I., RAHMAN K., BENISTON M., 2014, Streamflow timing of mountain rivers in Spain: recent changes and future projections, Journal of Hydrology, vol. 517, p. 1114–1127. http://dx.doi.org/10.1016/j.jhydrol.2014.06.053

MUNIA H., GUILLAUME J. H. A., MIRUMACHI N., PORKKA M., WADA Y., KUMMU M., 2016, Water stress in global transboundary river basins: significance of upstream water use on downstream stress, Environmental Research Letters, vol. 11, n° 1, 014002. https://doi.org/10.1088/1748-9326/11/1/014002

OCTAVIANTI T., STADDON C., 2021, A review of 80 assessment tools measuring water security, WIREs Water, vol. 8, n° 3, e1516. https://doi.org/10.1002/wat2.1516

ORT C., HOLLENDER J., SCHAERER M., SIEGRIST H.R., 2009, Model-based evaluation of reduction strategies for micropollutants from wastewater treatment plants in complex river networks, Environmental Science & Technology, vol. 43, n° 9, p. 3214–3220. https://doi.org/10.1021/es802286v

PAHL-WOSTL C., PALMER M., RICHARDS K., 2013, Enhancing water security for the benefits of humans and nature—the role of governance, Current Opinion in Environmental Sustainability, vol. 5, p. 676–684. https://doi.org/10.1016/j.cosust.2013.10.018

PAHL-WOSTL C., BHADURI A., GUPTA J., 2016, Water security: a popular but contested concept, in PAHL-WOSTL C., BHADURI A. (eds), Handbook on Water Security, Edward Elgar Publishing. p. 1–16. https://doi.org/10.4337/9781782548010.00006

PEDRO-MONZONÍS M., SOLERA A., FERRER J., ESTRELA T., PAREDES-ARQUIOLA J., 2015, A review of water scarcity and drought indexes in water resources planning and management, Journal of Hydrology, vol. 527, p. 482–493. https://doi.org/10.1016/j.jhydrol.2015.05.003

PROCLIM, 2005, Hitzesommer 2003, Synthesebericht, ProClim – Forum for Climate and Global Change (Ed.), Bern, 28 p. ISBN: 978-3-907630-16-7. (in German)

QI C., CHANG N-B., 2011, System dynamics modeling for municipal water demand estimation in an urban region under uncertain economic impacts, Journal of Environmental Management, vol. 92, n° 6, p. 1628–1641. https://doi.org/10.1016/j.jenvman.2011.01.020

REYNARD E., BONRIPOSI M., GRAEFE O., HOMEWOOD C., HUSS M., KAUZLARIC M., LINIGER H., REY E., RIST S., SCHÄDLER B., SCHNEIDER F., WEINGARTNER R., 2014a, Interdisciplinary assessment of complex regional water systems and their future evolution: how socioeconomic drivers can matter more than climate: Interdisciplinary assessment of complex regional water systems and their future evolution, WIREs Water, vol. 1, n° 4, p. 413–426. https://doi.org/10.1002/wat2.1032

REYNARD E., GRAEFE O., WEINGARTNER R., 2014b, Projet MontanAqua : les principaux résultats ou comment communiquer avec les acteurs locaux, Aqua & Gas, vol. 11, 50-57.

RINAUDO J.-D., 2015, Long-term water demand forecasting, in GRAFTON Q. et al. (eds), Understanding and managing urban water in transition, Global Issues in Water Policy, vol. 15, p. 239–268. https://doi.org/10.1007/978-94-017-9801-3_11

ROBINSON C. T., SCHUWIRTH N., BAUMGARTNER S., STAMM C., 2014, Spatial relationships between land-use, habitat, water quality and lotic macroinvertebrates in two Swiss catchments, Aquatic Sciences, vol. 76, n° 3, p. 375–392. https://doi.org/10.1007/s00027-014-0341-z

ROMANO G., SALVATI N., GUERRINI A., 2014, Estimating the determinants of residential water demand in Italy, Water, vol. 6, p. 2929-2945. https://doi.org/10.3390/w6102929

SAULNIER G.-M., CASTAINGS W., HOHENWALLNER D., BRANCELJ A. et al., 2011, Monitoring and modelling of mountain water resources. A short guideline based on the results of Alp-Water-Scarce, Technical report Alp-Water-Scarce (Interreg IV B, Alpine Space Programme, project 5-1-3-F). 47p.

SAUTIER J.-L., 2004, Water supply in the “Parc jurassien vaudois”, Géomatique Suisse : géoinformation et gestion du territoire, vol. 102, n° 6, p. 355–357 (in French).

SAVENIJE H.H.G., VAN DER ZAAG P., 2008, Integrated water resources management: Concepts and issues, Physics and Chemistry of the Earth, Parts A/B/C, vol. 33, p. 290–297. https://doi.org/10.1016/j.pce.2008,02.003

SCHERRER S. C., FISCHER E. M., POSSELT R., LINIGER M. A., CROCI-MASPOLI M., KNUTTI R., 2016, Emerging trends in heavy precipitation and hot temperature extremes in Switzerland: trends in Swiss climate extremes, Journal of Geophysical Research: Atmospheres, vol. 121, n° 6, p. 2626–2637. https://doi.org/10.1002/2015JD024634

SCHLEICH J., HILLENBRAND T., 2009, Determinants of residential water demand in Germany, Ecological Economics, vol. 68, n° 6, p. 1756-1769. https://doi.org/10.1016/j.ecolecon.2008.11.012

SCHMIDLI J., FREI C., 2005. Trends of heavy precipitation and wet and dry spells in Switzerland during the 20th century, International Journal of Climatology, vol. 25, n° 6, p. 753–771. https://doi.org/10.1002/joc.1179

SCHNEIDER F., HOMEWOOD C., 2013, Exploring water governance arrangements in the Swiss Alps from the perspective of adaptive capacity, Mountain Research and Development, vol. 33, n° 3, p. 225–233. https://doi.org/10.1659/MRD-JOURNAL-D-13-00004.1

SCHNEIDER F., RIST S., 2014, Envisioning sustainable water futures in a transdisciplinary learning process: combining normative, explorative, and participatory scenario approaches, Sustainability Science, vol. 9, n° 4, p. 463-481. https://doi.org/10.1007/s11625-013-0232-6

SCHNEIDER F., BONRIPOSI M., GRAEFE O., HERWEG K., HOMEWOOD C., HUSS M., KAUZLARIC M., LINIGER H., REY E., REYNARD E., RIST S., SCHÄDLER B., WEINGARTNER R., 2015, Assessing the sustainability of water governance systems: the sustainability wheel, Journal of Environmental Planning and Management, vol. 58, n° 9, p. 1577–1600. https://doi.org/10.1080/09640568.2014.938804

SHIKLOMANOV I.A., 1991, The world's water resources, Proc. Int. Symp. To Commemorates 25 Years of the IHP. UNESCO/IHP, Paris, France, 93–126.

SIVAPALAN M., SAVENIJE H., BLÖSCHL G., 2012, Socio-hydrology: A new science of people and water, Hydrological Processes, vol. 26, n° 8, p. 1270–1276. https://doi.org/10.1002/hyp.8426

SGWA – SWISS GAS AND WATER INDUSTRY ASSOCIATION, 2004, Water Distribution Data. www.qualitedeleau.ch (Accessed 11.2019).

STANGHELLINI L., COLLENTINE D., 2008, Stakeholder discourse and water management implementation of the participatory model CATCH in a Northern Italian alpine sub-catchment, Hydrology and Earth System Sciences, vol. 12, n° 1, p. 317–331. https://doi.org/10.5194/hess-12-317-2008

STATISTIQUE VAUD, 2011, Population perspectives 2010–2040. Vaud and Its Regions, Statistique Vaud, Service cantonal de recherche et d'information statistiques 54 p. (in French).

STEWART I., 2009, Changes in snowpack and snowmelt runoff for key mountain regions, Hydrological Processes, vol. 23, p. 78–94. http://dx.doi.org/10.1002/hyp.7128

SULLIVAN C., 2002, Calculating a Water Poverty Index, World Development, vol. 30, p. 1195–1210. https://doi.org/10.1016/S0305-750X(02)00035-9

SUN F., STADDON C., CHEN M. 2016, Developing and applying water security metrics in China: experience and challenges, Current Opinion in Environmental Sustainability, vol. 21, p. 29–36. https://doi.org/10.1016/j.cosust.2016.10.006

UN WATER, 2013, Water security & the global water agenda. A UN-Water Analytical Brief, Ontario, Canada, United Nations University. ISBN 978-92-808-6038-2

UNESCO-IHP, 2012, Strategic Plan of the eigth phase of IHP (International Hydrological Programme), « Water security: responses to local, regional, and global challenges », Strategic plan, Draft, 50 p. Paris, France, UNESCO-IHP

VANHAM D., FLEISCHHACKER E., RAUCH W., 2009, Impact of an extreme dry and hot summer on water supply security in an alpine region, Water Science & Technology, vol. 59, n° 3, p. 469–477. https://doi.org/10.2166/wst.2009,887

VANHAM D., MILLINGER S., PLIESSNIG H., RAUCH W., 2011, Rasterised water demands: methodology for their assessment and possible applications, Water Resources Management, vol. 25, p. 3301–3320. https://doi.org/10.1007/s11269-011-9857-3

VANHAM D., HOEKSTRA A. Y., WADA Y., BOURAOUI F., DE ROO A., MEKONNEN M. M., VAN DE BUND W., BATELAAN O., PAVELIC P., BASTIAANSSEN W., KUMMU M., ROCKSTRÖM J., LIUM J., BISSELINK B., RONCO P., PISTOCCHI A., BIDOGLIO G., 2018, Physical water scarcity metrics for monitoring progress towards SDG target 6.4: An evaluation of indicator 6.4.2 “Level of water stress”, Science of the Total Environment, vol. 613614, p. 218–232. https://doi.org/10.1016/j.scitotenv.2017.09.056

VAN VLIET M., FLÖRKE M., WADA Y., 2017, Quality matters for water scarcity. Nature Geoscience, vol. 10, n° 11, p. 800–802. https://doi.org/10.1038/ngeo3047

VARELA-ORTEGA C., BLANCO-GUTIÉRREZ I., SWARTZ C., DOWNING T., 2011, Balancing groundwater conservation and rural livelihoods under water and climate uncertainties: An integrated hydroeconomic modeling framework, Global Environmental Change, vol. 21, p. 604–619. https://doi.org/10.1016/j.gloenvcha.2010.12.001

VIVIROLI D., WEINGARTNER R., 2004, The hydrological significance of mountains: from regional to global scale, Hydrology and Earth System Sciences, vol. 8, n° 6, p. 1017–1030. https://doi.org/10.5194/hess-8-1017-2004

VIVIROLI D., ZAPPA M., GURTZ J., WEINGARTNER R., 2009, An introduction to the hydrological modelling system PREVAH and its pre- and post-processing-tools, Environmental Modelling & Software, vol. 24, p. 1209–1222. https://doi.org/10.1016/j.envsoft.2009,04.001

WADA Y., VAN BEEK L., BIERKENS M., 2011, Modelling global water stress of the recent past: on the relative importance of trends in water demand and climate variability. Hydrology and Earth System Sciences, vol. 15, n° 12, p. 3785–3808. https://doi.org/10.5194/hess-15-3785-2011

WANG X., ZHANG J., SHAHID S., GUAN E., WU Y., GAO J., HE R., 2016, Adaptation to climate change impacts on water demand, Mitigation and Adaptation Strategies for Global Change, vol. 21, n° 1, p. 81–99. https://doi.org/10.1007/s11027-014-9571-6

WARD D., MCKAGUE, K., 2007, Water requirements of livestock, Factsheet Order No. 07-023. Ministry of Agriculture, Food and Rural Affairs, Ontario (Canada). ISSN 1198-712X

WEINGARTNER R., SCHÄDLER B., REYNARD E., BONRIPOSI M., GRAEFE O., HERWEG K., HOMEWOOD C., HUSS M., KAUZLARIC M., LINIGER H., REY E., RIST S., SCHNEIDER F., 2014, MontanAqua: Wasserbewirtschaftung in Zeiten von Knappheit und globalem Wandel, Wasserbewirtschaftungsoptionen für die Region Crans-Montana-Sierre im Wallis, Forschungsbericht des Nationalen Forschungsprogramms NFP 61, Bern (in German).

WHEATER H., 2015, Water Security – science and management challenges, Proceedings of the International Association of Hydrological Sciences, vol. 366, p. 23–30. https://doi.org/10.5194/piahs-366-23-2015

WIEK A., LARSON K., 2012, Water, people, and sustainability – A systems framework for analyzing and assessing water governance regimes, Water Resources Management, vol. 26, p. 3153–3171. https://doi.org/10.1007/s11269-012-0065-6

YOUNG G., DEMUTH S., MISHRA A., CUDENNEC C., 2015, Hydrological sciences and water security: An overview, Proceedings of the International Association of Hydrological Sciences, vol. 366, p. 1–9. https://doi.org/10.5194/piahs-366-1-2015

ZENG Z., LIU J., SAVENIJE H., 2013, A simple approach to assess water scarcity integrating water quantity and quality, Haut de page

Notes

1 MontanAqua (2010-2014), financed by the Swiss National Foundation, and ICCARE-Vaud (2013-2015), financed by the University of Lausanne.

2 Quantifier les usages de l’eau en territoire touristique de montagne (2013-2018), PhD thesis financed by the University of Lausanne (Calianno, 2018), and LABEAU : Mise en place d’un observatoire des usages de l’eau à l’échelle régionale (2020-2021), financed by the University of Lausanne, the BlueArk innovation pole and ALTIS SA water company.

3 The municipalities of Bagnes and Vollèges merged on 1st January 2021 to form the commune of Val de Bagnes. Our study focused on the municipality of Bagnes before the fusion.

4 In the canton of Vaud, hydropower is mainly run-of-river production and is highly regulated by long-term concessions. Artificial snow production is restricted to Alpine catchments, which are not considered in this study. These two water users were hence not taken into account in this study.

5 As this use is strictly regulated by long-term concessions (and therefore does not influence the water needs of specific groups of stakeholders), it was not included in our calculations of the current and future water needs.

6 After 2060, the glacier will be too small to continue having a positive impact on river flows.

Haut de page

Table des illustrations

Titre Figure 1: Geographical location of the (1) Venoge, (2) Talent and (3) Grande Eau catchments, the (4) Crans-Montana-Sierre area and (5) the municipality of Bagnes
Légende VD – canton of Vaud, VS – canton of Valais. The dashed lines show the borders of the catchments studied in the ICCARE-Vaud project (Milano et al., 2015a,b) but not presented in this paper.
URL http://journals.openedition.org/geocarrefour/docannexe/image/18618/img-1.png
Fichier image/png, 535k
Titre Figure 2: Methodological approach
Légende In black: methodology core, in grey: additional data for future state assessment. P: Precipitation, T: Temperature
URL http://journals.openedition.org/geocarrefour/docannexe/image/18618/img-2.png
Fichier image/png, 82k
Titre Figure 3: Current and future water scarcity in catchments of the canton of Vaud and in the Crans-Montana-Sierre area based on the water scarcity index
Crédits Source: Shiklomanov, 1991
URL http://journals.openedition.org/geocarrefour/docannexe/image/18618/img-3.png
Fichier image/png, 94k
Titre Figure 4: Changing trends in water resources in western Switzerland
URL http://journals.openedition.org/geocarrefour/docannexe/image/18618/img-4.png
Fichier image/png, 145k
Haut de page

Pour citer cet article

Référence électronique

Marianne Milano et Emmanuel Reynard, « Prospective integrated modelling of water scarcity risk in western Switzerland: lessons learned and new challenges for water security assessment », Géocarrefour [En ligne], 96/1 | 2022, mis en ligne le 28 juin 2022, consulté le 08 août 2022. URL : http://journals.openedition.org/geocarrefour/18618 ; DOI : https://doi.org/10.4000/geocarrefour.18618

Haut de page

Auteurs

Marianne Milano

Université de Lausanne, Institut de géographie et durabilité et Centre interdisciplinaire de recherche sur la montagne, Géopolis, CH-1015 Lausanne marianne.milano@unil.ch

Emmanuel Reynard

Université de Lausanne, Institut de géographie et durabilité et Centre interdisciplinaire de recherche sur la montagne, Géopolis, CH-1015 Lausanne emmanuel.reynard@unil.ch

Articles du même auteur

Haut de page

Droits d’auteur

Tous droits réservés

Haut de page
  • OpenEdition Journals
Rechercher dans OpenEdition Search

Vous allez être redirigé vers OpenEdition Search