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Changing climate and human demographics in the world's mountains will have increasingly profound environmental and societal consequences across all elevations. Quantifying current human populations in and near mountains is crucial to ensure that any interventions in these complex social-ecological systems are appropriately resourced, and that valuable ecosystems are effectively protected. However, comprehensive and reproducible analyses on this subject are lacking. Here, we develop and implement an open workflow to quantify the sensitivity of mountain population estimates over recent decades, both globally and for several sets of relevant reporting regions, to alternative input dataset combinations. Relationships between mean population density and several potential environmental covariates are also explored across elevational bands within individual mountain regions (i.e. "sub-mountain range scale"). Globally, mountain population estimates vary greatly-from 0.344 billion (5% of the corresponding global total) to 2.289 billion (31%) in 2015. A more detailed analysis using one of the population datasets (GHS-POP) revealed that in ∼35% of mountain sub-regions, population increased at least twofold over the 40-year period 1975-2015. The urban proportion of the total mountain population in 2015 ranged from 6% to 39%, depending on the combination of population and urban extent datasets used. At sub-mountain range scale, population density was found to be more strongly associated with climatic than with topographic and protected-area variables, and these relationships appear to have strengthened slightly over time. Such insights may contribute to improved predictions of future mountain population distributions under scenarios of future climatic and demographic change. Overall, our work emphasizes that irrespective of data choices, substantial human populations are likely to be directly affected by-and themselves affect-mountainous environmental and ecological change. It thereby further underlines the urgency with which the multitudinous challenges concerning the interactions between mountain climate and human societies under change must be tackled.

The Hindu Kush Himalaya (HKH) is the pulse of the planet. Being at the top of the world, changes happen here before anywhere else, and its beat vibrates across the globe. But urgent actions are required to ensure the health of this global asset and the wellbeing of its people. The uniqueness of HKH mountain people should be recognized and prioritized, and ecosystem services protected by halting biodiversity loss and land degradation. The implementation of the Sustainable Development Goals in the HKH needs to become a global top priority, and keeping global warming below the ambitious 1.5°C target is especially urgent here. To achieve all of this, more sharing of information and more robust regional cooperation are required. These 6 urgent actions summarize the HKH Call to Action, formulated through a rigorous consultative process coordinated by the International Centre for Integrated Mountain Development in the 8 HKH countries, based on the key findings of the Hindu Kush Himalaya Assessment report [ https://link.springer.com/book/10.1007%2F978-3-319-92288-1].

This article shows how large-scale commercial farmers, individually and collectively, are responding to land and water reform processes in the Thukela River basin, KwaZulu-Natal, South Africa. With a high degree of innovative agency, commercial farmers have effectively executed four strategies, enabling them to adapt and use their access to resources to neutralize multiple water reform efforts that once promised to be catalysts for inclusive change in the post-apartheid era. It is likely that policy alone will not facilitate the envisioned transformation, if local practices are not sufficiently understood and anticipated by the governmental officials charged with the implementation of water reform processes.

The article analyzes Tidal River Management in Bangladesh from a social learning perspective. Four cases were investigated using participatory assessment. Knowledge acquisition through transformations in the Tidal River Management process was explored as an intended learning outcome. The study finds that social learning occurred more prominently at the individual stakeholder level and less at the collective level. For Tidal River Management to be responsive and sustainable, especially in times of increased uncertainty and climate vulnerability, more attention needs to be paid to coordination and facilitation of multi-level learning that includes all stakeholders.

This article traces a policy shift that makes the ‘water user’ the main subject of water governance. From a Foucauldian perspective on governmentality these new subjectivities accompany neo-liberal governmental technologies to devolve autonomy from state institutions to an active user base, whilst retaining some ‘control at a distance’. The expectation is that individual subjects will incorporate control mechanisms and internalize norms and that this leads to new publicly auditable forms of self-regulation. The article questions the underlying assumption that policy necessarily accomplishes its strategic effects through governmentality. For this purpose, it draws on an ethnographic case study of how policy produced a new power/knowledge regime and how different societal actors and ‘user’ groups responded to that. The study specifically investigates the Mexican policy of irrigation management transfer during the 1990s, by which government transferred the public control over irrigation districts to locally organized water users’ associations (WUAs). The article argues that governmental technologies make and govern the ‘water user’ by discursively and materially constituting an organizational arrangement for user management (WUA), more than by directly acting on individuals’ self-regulated conduct. The analysis contributes to a broader reflection on the role of power/knowledge in natural resources management and decentralized resources governance.

The reality of global climate change demands novel approaches to science that are reflective of the scales at which changes are likely to occur, and of the new forms of knowledge required to positively influence policy to support vulnerable populations. We examine some of the opportunities and challenges presented by a collaborative, transdisciplinary research project on climate change adaptation in Africa and Asia that utilised a hotspot approach. A large scale effort to develop appropriate baselines was a key challenge at the outset of the program, as was the need to develop innovative methodologies to enable researchers to work at appropriate spatial scales. Efforts to match research to the biophysical scales at which change occurs need to be aware of the mismatch that can develop between these regional scales and the governance scales at which decisions are made.

Densely populated floodplains downstream of Asia’s mountain ranges depend heavily on mountain water resources, in particular for irrigation. An intensive and complex multi-cropping irrigated agricultural system has developed here to optimize the use of these mountain water resources in conjunction with monsoonal rainfall. Snow and glacier melt thereby modulate the seasonal pattern of river flows and, together with groundwater, provide water when rainfall is scarce. Climate change is expected to weaken this modulating effect, with potentially strong effects on food production in one of the world’s breadbaskets. Here we quantify the space-, time- and crop-specific dependence of agriculture in the Indo-Gangetic Plains on mountain water resources, using a coupled state-of-the-art, high-resolution, cryosphere–hydrology–crop model. We show that dependence varies strongly in space and time and is highest in the Indus basin, where in the pre-monsoon season up to 60% of the total irrigation withdrawals originate from mountain snow and glacier melt, and that it contributes an additional 11% to total crop production. Although dependence in the floodplains of the Ganges is comparatively lower, meltwater is still essential during the dry season, in particular for crops such as sugar cane. The dependency on meltwater in the Brahmaputra is negligible. In total, 129 million farmers in the Indus and Ganges substantially depend on snow and glacier melt for their livelihoods. Snow and glacier melt provides enough water to grow food crops to sustain a balanced diet for 38 million people. These findings provide important information for agricultural and climate change adaptation policies in a climate change hot spot where shifts in water availability and demand are projected as a result of climate change and socio-economic growth. Climate change will affect Himalayan water resources. This study quantifies the importance of snow and glacier melt for agriculture on the Indo-Gangetic plain, finding that 129 million farmers depend on it, especially for rice and cotton, and that meltwater supports crops feeding 38 million people.

Studies of climate change at specific intervals of future warming have primarily been addressed through top-down approaches using climate projections and modelled impacts. In contrast, bottom-up approaches focus on the recent past and present vulnerability. Here, we examine climate signals at different increments of warming and consider the need to reconcile top-down and bottom-up approaches. We synthesise insights from recent studies in three climate-sensitive systems where change is a defining feature of the human-environment system. Whilst top-down and bottom-up approaches generate complementary insights into who and what is at risk, integrating their results is a much-needed step towards developing relevant information to address the needs of immediate adaptation decisions.

Mountains are large landforms raised above the surface of the earth emerging into peaks and ranges. Mountains occupy 22% of the world’s land surface area and are home to about 13% of the world’s population (FAO 2015). While about 915 million people live in mountainous region, less than 150 million people live above 2,500 m above sea level (masl), and only 20–30 million people live above 3,000 masl.

The International Centre for Integrated Mountain Development is coordinating the Hindu Kush Himalayan Monitoring and Assessment Programme, which will be carried out with partners and individual experts. The assessment addresses the social, economic, and environmental pillars of sustainable mountain development and will serve as a basis for evidence-based decision-making to safeguard the environment and advance people’s wellbeing. It is not a one-off assessment but will be an ongoing process. A 2017 publication is planned as the first of a series of monitoring and assessment reports.

We define and explore hydrosocial territories as spatial configurations of people, institutions, water flows, hydraulic technology and the biophysical environment that revolve around the control of water. Territorial politics finds expression in encounters of diverse actors with divergent spatial and political-geographical interests. Their territory-building projections and strategies compete, superimpose and align to strengthen specific water-control claims. Thereby, actors continuously recompose the territory’s hydraulic grid, cultural reference frames, and political-economic relationships. Using a political ecology focus, we argue that territorial struggles go beyond battles over natural resources as they involve struggles over meaning, norms, knowledge, identity, authority and discourses.

The Indus, Ganges, and Brahmaputra (IGB) river basins provide about 900 million people with water resources used for agricultural, domestic, and industrial purposes. These river basins are marked as climate change hotspot, where climate change is expected to affect monsoon dynamics and the amount of meltwater from snow and ice, and thus the amount of water available. Simultaneously, rapid and continuous population growth, and strong economic development will likely result in a rapid increase in water demand. Since quantification of these future trends is missing, it is rather uncertain how the future South Asian water gap will develop. To this end, we assess the combined impacts of climate change and socio-economic development on future blue water scarcity for the IGB until the end of the 21st century. We apply a coupled modelling approach consisting of the distributed cryospheric-hydrological model SPHY, which simulates current and future upstream water supply, and the hydrology and crop production model LPJmL, which simulates current and future downstream water supply and demand. We force the models with an ensemble of eight representative downscaled General Circulation Models (GCMs) that are selected from the RCP4.5 and RCP8.5 scenarios, and a set of land use and socio-economic scenarios that are consistent with the Shared Socio-economic Pathway (SSP) marker scenarios 1 and 3. The simulation outputs are used to analyse changes in water availability, supply, demand, and scarcity. The outcomes show an increase in surface water availability towards the end of the 21st century, which can mainly be attributed to increases in monsoon precipitation. However, despite the increase surface water availability, the strong socio-economic development and associated increase in water demand will likely lead to an increase in the water gap during the 21st century. This indicates that socio-economic development is the key driver in the evolution of the future South Asian water gap.

Water International is the official journal of the International Water Resources Association (IWRA), and like its parent is dedicated to collaborative advancement and dissemination of knowledge on ...

Around the world it has proven very difficult to develop policies and interventions that ensure socio-environmentally sustainable groundwater use and exploitation. In the state of Guanajuato, Central Mexico, both the national government and the decentralized state government have pursued to regulate groundwater use through direct state control, groundwater markets, energy pricing, and user self-regulation. We present and analyze these regulatory mechanisms and their outcomes in the field. We argue that the close interdependencies of these regulatory mechanisms have pre-empted the effectiveness of these policy instruments as well as that of other measures aimed at reducing groundwater use in order to advance towards sustainable exploitation levels.

Both civil engineering and environmentalism strongly influenced the development of water governance in the Netherlands in the 20th century. Much research has focused on these aspects separately. This article maps the interaction between governance, technology and ecological systems in the Netherlands, to provide insights into how these are co-evolving. The analysis is based on a combination of a literature study and an empirical case study on the debates concerning the reopening of the Philipsdam, in the Southwest Delta of the Netherlands. It shows how the negotiations that took place in constructing facts in the Philipsdam case both increased the complexity of decision-making concerning the dam itself and radiated outwards to affect other parts of the Dutch water system. We conclude that the process of constructing facts and the way these are framed once they have been established as facts are both intrinsically political and reflect the multiplicity of views of how the lake works and what the problem is, and how these views are incompatible at times. As such, ontological complexity is ingrained in what is represented as facts and severely complicates an apparently matter of fact decision to reopen a dam.

This paper applies an ontological politics approach for studying how complexity, uncertainty, and ignorance are being dealt with in the Netherlands by looking at how knowledges are produced and incorporated in decision-making on uncertain climate change. On the basis of work done in the Netherlands, this paper shows two things in particular. First, how decision making responses historically have been subject to change under the influence of floods and how the emergence of climate change has significantly changed these floods. Second, based on the analysis of processes dealing with a blue-green algae problem in a lake, climate change not only changed decision making responses but also changed the very reality that is being enacted. Consequently, this brings an ethical dimension to the fore, related to the intrinsic tension between the growing awareness that “all is interconnected” on the one hand and the realization we cannot take all into account.

This article reviews, illustrated by two case studies, how struggles around scales play out in three globally hegemonic trends in river governance: (1) stakeholder participation for (2) integrated water resources management (IWRM), conceived at (3) the watershed or river basin level. This ‘holy trinity’[1] has found blanket acceptance and support both in top-down (donors, governments) and bottom-up [nongovernmental organizations (NGOs)] directions as a way of democratizing water management, rationalizing water resource use, and managing conflict between water users in river basins. The precepts underlying these trends however have largely gone unquestioned, and the basin scale has become ‘naturalized’. This continuing hegemonic frame tends to obfuscate how boundaries are often manipulated for political ends and how different stakeholders frame the ‘natural’ scale in quite different ways. In this article we notably question the way boundaries get drawn and scales framed in light of water infrastructure, such as dams, canals, locks, and pipelines, which not only act as ‘pipelines of power’ but also seemingly impose management scale, ‘naturalizing’ water management in a different, semi-deterministic way. Rather than providing a full-fledged literature review, we build our argument drawing from cases from Ecuador and Turkey, each in its own way showing that depoliticizing discourse hides a political reality that may be better captured by ‘polycentricity’.

The promotion of local governance and the transfer of water management responsibilities to water user associations (WUAs) have been central in water reform processes throughout the world, including in the reforms that took place in post-apartheid South Africa. This paper reflects on the notions of inclusion and representation as put forward by the various actors involved in the establishment of a WUA in a tertiary catchment in the Thukela River Basin. The paper describes how the WUA in the study catchment came to be dominated by commercial farmers, despite the South African government's aim to redress the inequities of the past by the inclusion and representation of historically disadvantaged individuals. The authors argue that the notions of inclusion and representation as embedded in the concept of the WUA are highly contested and more aligned with the institutional settings familiar to the commercial farmers. The paper concludes that, unless the inherently political nature of the participatory process is recognized and the different institutional settings become part of the negotiation process of the ‘why’ and the ‘how’ of progressive collaboration at catchment level, the establishment of the WUA in the study catchment will not contribute to achieving the envisioned transformation.

The cryosphere reacts sensitively to climate change, as evidenced by the widespread retreat of mountain glaciers. Subsurface ice contained in permafrost is similarly affected by climate change, causing persistent impacts on natural and human systems. In contrast to glaciers, permafrost is not observable spatially and therefore its presence and possible changes are frequently overlooked. Correspondingly, little is known about permafrost in the mountains of the Hindu Kush Himalaya (HKH) region, despite permafrost area exceeding that of glaciers in nearly all countries. Based on evidence and insight gained mostly in other permafrost areas globally, this review provides a synopsis on what is known or can be inferred about permafrost in the mountains of the HKH region. Given the extreme nature of the environment concerned, it is to be expected that the diversity of conditions and phenomena encountered in permafrost exceed what has previously been described and investigated. We further argue that climate change in concert with increasing development will bring about diverse permafrost-related impacts on vegetation, water quality, geohazards, and livelihoods. To better anticipate and mitigate these effects, a deepened understanding of high-elevation permafrost in subtropical latitudes as well as the pathways interconnecting environmental changes and human livelihoods are needed. © Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License.

The impacts of climate change on people’s livelihoods have been widely documented.1 It is expected that climate and environmental change will hamper poverty reduction, or even exacerbate poverty in some or all of its dimensions. Changes in the biophysical environment, such as droughts, flooding, water quantity and quality, and degrading ecosystems, are expected to affect opportunities for people to generate income. These changes, combined with a deficiency in coping strategies and innovation to adapt to particular climate change threats, are in turn likely to lead to increased economic and social vulnerability of households and communities, especially amongst the poorest.

Climate change impact studies depend on projections of future climate provided by climate models. The number of climate models is large and increasing, yet limitations in computational capacity make it necessary to compromise the number of climate models that can be included in a climate change impact study. The selection of climate models is not straightforward and can be done by following different methods. Usually, the selection is either based on the entire range of changes in climatic variables as projected by the total ensemble of available climate models or on the skill of climate models to simulate past climate. The present study combines these approaches in a three-step sequential climate model selection procedure: (1) initial selection of climate models based on the range of projected changes in climatic means, (2) refined selection based on the range of projected changes in climatic extremes and (3) final selection based on the climate model skill to simulate past climate. This procedure is illustrated for a study area covering the Indus, Ganges and Brahmaputra river basins. Subsequently, the changes in climate between 1971–2000 and 2071–2100 are analysed, showing that the future climate projections in this area are highly uncertain but that changes are imminent.

Direct groundwater regulation (e.g. registration of abstraction points, permits and concessions) has been much advocated world-wide; however, few successful cases have been reported. The development of groundwater use in Minqin County, Gansu Province, China, is described, with analyses of the situation before and after the implementation of direct groundwater regulation measures in 2007. Based on a survey carried out in 2010, it is argued that the regulation measures, which were part of a broader water-policy reform, were successfully implemented due to their integration with pre-existing collective groundwater institutions. In addition to the regulation measures—the closure of wells and per capita water use restriction—all villages had to form water users’ associations (WUAs) which were assigned to implement the new regulations. These WUAs were found to have the same structure as the existing collective groundwater institutions. Through the water-policy reform, the function of the pre-existing groundwater institutions was transformed from managing “water exploitation” to managing “water conservation”.

Collective groundwater management by water users—self-regulation—is increasingly advocated as a complement to state regulation. This article analyzes the attempts by the Guanajuato State Water Commission (CEAG) in central Mexico to promote user self-regulation through the establishment and development of 14 Consejos Tecnicos de Aguas (COTAS; Technical Water Councils). Based on a joint assessment by a former senior CEAG policy-maker and two researchers, Guanajuato’s groundwater-management policy is reviewed to understand why user self-regulation was less successful than expected. It concludes that increasing awareness and improving the knowledge base on groundwater is not enough to trigger self-regulation by groundwater users. A wider delegation of responsibilities to the COTAS is necessary, combined with: (1) functioning mechanisms for enforcing groundwater legislation, especially concerning well permits and pumped volumes, and (2) mechanisms that ensure the legitimacy and accountability of users’ representatives to both users and state agencies.

An increasing number of research programs seek to support adaptation to climate change through the engagement of large‐scale transdisciplinary networks that span countries and continents. While transdisciplinary research processes have been a topic of reflection, practice, and refinement for some time, these trends now mean that the global change research community needs to reflect and learn how to pursue collaborative research on a large scale. This paper shares insights from a seven‐year climate change adaptation research program that supports collaboration between more than 450 researchers and practitioners across four consortia and 17 countries. The experience confirms the importance of attention to careful design for transdisciplinary collaboration, but also highlights that this alone is not enough. The success of well‐designed transdisciplinary research processes is also strongly influenced by relational and systemic features of collaborative relationships. Relational features include interpersonal trust, mutual respect, and leadership styles, while systemic features include legal partnership agreements, power asymmetries between partners, and institutional values and cultures. In the new arena of large‐scale collaborative science efforts, enablers of transdisciplinary collaboration include dedicated project coordinators, leaders at multiple levels, and the availability of small amounts of flexible funds to enable nimble responses to opportunities and unexpected collaborations.

Flood-risk management (FRM) is shaped by context: a society’s cultural background; physical possibilities and constraints; and the historical development of that society’s economy, politi- cal system, education, etc. These provide different drivers for change, in interaction with more global developments. We compare historical and current FRM in six delta areas and their con- texts: Rhine/Meuse/Scheldt (The Netherlands), Pearl River (China), Mekong (Vietnam), Ganges/ Brahmaputra/Meghna (Bangladesh) Zambezi/Limpopo (Mozambique), and Mississippi (USA). We show that in many countries the emphasis is shifting from ‘hard’ engineering, such as dikes, towards non-structural ‘soft’ measures, such as planning restrictions or early warning systems, while the ‘hard’ responses are softened in some by a ‘building with nature’ approach. However, this is by no means a universal development. One consistent feature of the application of ‘hard’ FRM technology to deltas is that it pushes them towards a technological ‘lock-in’ in which fewer and fewer ‘soft’ FRM alternatives are feasible due to increased ood risks. By contrast, ‘soft’ FRM is typically exible, allowing a range of future options, including future hard elements if needed and appropriate. These experiences should lead to serious re ection on whether ‘hard’ FRM should be recommended when ‘soft’ FRM options are still open.

The extent and distribution of permafrost in the mountainous parts of the Hindu Kush Himalayan (HKH) region are largely unknown. A long tradition of permafrost research, predominantly on rather gentle relief, exists only on the Tibetan Plateau. Two permafrost maps are available digitally that cover the HKH and provide estimates of permafrost extent, i.e., the areal proportion of permafrost: the manually delineated Circum-Arctic Map of Permafrost and Ground Ice Conditions (Brown et al., 1998) and the Global Permafrost Zonation Index, based on a computer model (Gruber, 2012). This article provides a first-order assessment of these permafrost maps in the HKH region based on the mapping of rock glaciers. Rock glaciers were used as a proxy, because they are visual indicators of permafrost, can occur near the lowermost regional occurrence of permafrost in mountains, and can be delineated based on high-resolution remote sensing imagery freely available on Google Earth. For the mapping, 4000 square samples (~ 30 km2) were randomly distributed over the HKH region. Every sample was investigated and rock glaciers were mapped by two independent researchers following precise mapping instructions. Samples with insufficient image quality were recorded but not mapped. We use the mapping of rock glaciers in Google Earth as first-order evidence for permafrost in mountain areas with severely limited ground truth. The minimum elevation of rock glaciers varies between 3500 and 5500 m a.s.l. within the region. The Circum-Arctic Map of Permafrost and Ground Ice Conditions does not reproduce mapped conditions in the HKH region adequately, whereas the Global Permafrost Zonation Index does so with more success. Based on this study, the Permafrost Zonation Index is inferred to be a reasonable first-order prediction of permafrost in the HKH. In the central part of the region a considerable deviation exists that needs further investigations.

Groundwater forms the basis for millions of rural and urban livelihoods around the world. Building on insights from the theory of access, in this article we present how groundwater development has brought much well-fare in many parts of the world; and how resulting intensive groundwater use is leading to ill-fare through aquifer overexploitation and processes of water accumulation and dispossession. We show the difficulty of state regulation and the modest achievements of other governance approaches that aim to solve existing groundwater problems. To study these processes we propose a framework of analysis that is based on the study of hydrosocial-networks, the political economy of groundwater and the domains and discourses that define groundwater access. Such analysis highlights the challenges of devising policies and modes of governance that contribute to social and environmental sustainability in intensively used aquifers. These we argue should build on an analysis of equity that scrutinizes the discourses, actors, powers and procedures that define groundwater access. By inciting debates on equity a first and fundamental step can be made toward advancing more inclusive groundwater governance that crucially engages the marginalized and addresses their groundwater problems, concerns and needs.

Through irrigation management transfer inMexico poorly functioning governancemechanisms for maintenance were replaced.New actors, new roles, and newresponsibilities in the maintenance ofMexican irrigation systems wereestablished. This article analyzes themaintenance service delivery mechanisms inthe Alto Rio Lerma Irrigation District(ARLID), to evaluate if and how theinstitutional arrangements establishedthrough management transfer ensure adequateservice provision. After presenting themain actors currently involved inirrigation maintenance, the rules andregulations underlying the servicerelationships between the actors involvedin maintenance in ARLID are analyzed. Thisis done by detailing how theserelationships are formally organized, howthey work in practice, and which incentivesexist for the service providers to providean efficient service and for the servicerecipient to pro-actively participate inservice provision. We conclude that the newinstitutional framework for maintenanceservice provision is quite coherent andthat the governance mechanisms that havebeen established work well, especiallythose between the farmers and theirorganizations. This has led to improvedmaintenance services.

In Molden, David (Ed.). Water for food, water for life: a Comprehensive Assessment of Water Management in Agriculture. London, UK: Earthscan; Colombo, Sri Lanka: International Water Management Institute (IWMI).

Through investigating the reactions of commercial farmers to land and water reforms in the Trichardtsdal-Ofcolaco area, Limpopo Province, Olifants Basin, South Africa, from 1997 to 2006, it is shown that water claims are key to land redistribution processes, and that commercial farmers make strategic use of arguments for nature conservation and ecological stewardship to defend their claims to water. Given these observations, caution is warranted with respect to the implementation of land and water reforms as separate policy packages; it may be more effective to design water and conservation policies as an integral part of land reform programmes.

Increasing water withdrawals for urban, industrial, and agricultural use have profoundly altered the hydrology of many major rivers worldwide. Coupled with degradation of water quality, low flows have induced severe environmental degradation and water has been rendered unusable by downstream users. When supply of water falls short of commitments to fulfil demand in terms of water quality and quantity within the basin and at the river mouth, for part or all of the year, basins are said to be closing. Basin closure is an anthropogenic process and manifested at societal as well as ecosystem levels, and both its causes and consequences are analyzed. Implications in terms of increased interconnectedness between categories of users and between societal processes and ecosystems in different parts of river basins are emphasized. Finally, several possible responses to the challenges posed by the over-exploitation of water resources are reviewed.

Introduction: Social Participation in Water Management and Governance Part I: Participation and Indigenous Water Governance 1. Participation of the Timbisha Shoshone Tribe in Land and Water Management Decisions in Death Valley National Park, California and Nevada, U.S. 2. For Whom the Turbines Turn: Indigenous Citizens as Legitimate Stakeholders in the Brazilian Amazon Part II: Participation and the Dynamics of Gender in Water Management 3. Gender and Participation in a Rural Water-Supply Organization in Rajasthan, India 4. Gendered Dynamics of Participation in Water Management in Nepal and Peru: Revisiting the Linkages between Membership and Power Part III: Participation and River Basin Governance 5. Social Participation in French Water Management: Contributions to River Basin Governance and New Challenges 6. Social Participation in Mexican River Basin Organizations: The Resilience of Coalitions 7. From a Participative Framework to Communities' Realities: The Challenges of Implementing Stakeholder Involvement in Quebec Watershed Management, Canada Part IV: Participation and Implementation of Water Management 8. Social Participation in the Irrigation Sector in Yunnan, China: Roles of the State, User Associations, and Communities 9. Participation in Water Resource and Service Governance in South Africa: Caught in the Acts 10. The Role of Locally-Managed Water Aid: Effective Partnerships in Sri Lanka 11. The Public's Role as Stakeholder in the Yarqon River Authority, Israel Part V: Participation and the Politics of Governance 12. Water Rights and Rule-Making Justice as Fruits of Social Struggle in the Ecuadorian Andes 13. Water Management Practices on Trial: The Tribunal Latinoameicano del Agua and the Creation of Public Space for Social Participation in Water Politics 14. The Local Application of Global Sustainable and Participatory Development Norms in Turkish Dams 15. Conclusions

Using a variety of case studies, this book provides an overview of how societies have gradually developed their water resources and furthers our understanding of how such resources can be managed successfully or unsuccessfully. Discussing how and why particular options are selected, and why a particular course of events eventually prevails, the book stresses the importance of context and a multidisciplinary approach in moving towards sustainable and equitable development.

Evidence of groundwater management by aquifer users emerging under Integrated Water Resources Management (IWRM) initiatives is presented, by analyzing the Consejos Técnicos de Aguas (COTAS; Technical Water Councils or Aquifer Management Councils) in the state of Guanajuato, Mexico, established between 1998 and 2000 by the Guanajuato State Water Commission (CEAG). Two contrasting models influenced this attempt to promote user self-regulation of groundwater extractions: locally autonomous aquifer organizations with powers to regulate groundwater extractions versus aquifer organizations with advisory powers only. The COTAS were conceived as locally autonomous IWRM organizations consisting of all aquifer users that would work together to reduce groundwater over-extraction and stabilize aquifer levels, at a later stage. CEAG followed an expedient IWRM approach to develop the COTAS, setting achievable targets for their development and explicitly focusing on active stakeholder participation. The article shows that, due to struggles between the state and federal levels, the COTAS have become advisory bodies that have not led to reductions in groundwater extractions. It concludes that achieving user self-regulation of groundwater extractions requires a fuller delegation of responsibilities to the COTAS which would not be possible without addressing the institutional struggles over water governance at the state and federal levels.

This chapter portrays the river basin trajectory of the Lerma-Chapala basin in central Mexico focusing on three periods (1500-1910, 1911-1980 and 1981 to the present). For each period, an analysis of the history of water development and the concomitant transformations in terms of water control and management are given. It analyses the relationship between basin closure and the hydraulic mission, defined as the strong conviction that the state should develop hydraulic infrastructure to capture as much water as possible for human uses. It focuses on the role of the hydrocracy (hydraulic bureaucracy) in the creation of water overexploitation in the basin.