Skip to main content Accessibility help
×
Hostname: page-component-7c8c6479df-995ml Total loading time: 0 Render date: 2024-03-28T23:25:16.250Z Has data issue: false hasContentIssue false

Chapter 6 - SDG 6: Clean Water and Sanitation – Forest-Related Targets and Their Impacts on Forests and People

Published online by Cambridge University Press:  02 December 2019

Pia Katila
Affiliation:
Natural Resources Institute Finland (Luke)
Carol J. Pierce Colfer
Affiliation:
Cornell University, New York and Center for International Forestry Research (CIFOR)
Wil de Jong
Affiliation:
Kyoto University, Japan
Glenn Galloway
Affiliation:
University of Florida
Pablo Pacheco
Affiliation:
World Wildlife Fund (WWF) and Center for International Forestry Research (CIFOR)
Georg Winkel
Affiliation:
European Forest Institute (EFI), Germany

Summary

Predicting the impact of SDG 6 on forests and forest people requires a balanced understanding of the relationship between forests and water. Notable aspects are that forest cover reduces annual runoff but correlates well with water quality, and that recycling of evapotranspiration from forests is important for downwind precipitation. Within this context a target-by-target review of SDG 6, informed by South American examples, suggests that the Goal is unlikely to exert a major influence on forest cover. Targets 6.1 and 6.2 concerning water and sanitation provision will have relatively little impact on forests except through a demand for hydrological ecosystem services and the use of wastewater in forestry. Within the four water resources targets (6.3–6.6) significant impacts may be limited to water efficiency considerations (Target 6.4) restricting plantations in water-stressed areas and Integrated Water Resources Management (Target 6.5) driving a more integrated view of catchments and their management. The eventual SDG 6 impact will depend on the context of water–forest relationships (illustrated using the Hindu Kush Himalayas as an example), the extent to which SDG 6 will in fact be implemented and alignment of the Goal with forest policies, based on a landscape approach.

Type
Chapter
Information
Publisher: Cambridge University Press
Print publication year: 2019
Creative Commons
Creative Common License - CCCreative Common License - BYCreative Common License - NC
This content is Open Access and distributed under the terms of the Creative Commons Attribution licence CC-BY-NC 4.0 https://creativecommons.org/cclicenses/

Key Points

  • SDG 6 seems unlikely to exert a major influence on forest cover and indeed is unlikely to be pursued with forests in the forefront of consideration.

  • Full implementation of Targets 6.1 and 6.2 could positively impact forest people, yet this is not an implementation priority.

  • SDG 6 may focus attention on the role of forests (as providers of hydrological ecosystems services) in protecting clean drinking water resources; the exact role of forests here requires careful consideration.

  • Particular attention should be given to reforestation strategies to improve water availability in areas with soil degradation and reduced infiltration. Target 6.4 may restrict the spread of new plantations in semi-arid areas and Target 6.5 may drive a more integrated view of catchments and their management.

  • It is necessary to consider forest–water interactions at the catchment, regional and continental scales; actions with a beneficial impact at one scale may have an adverse impact at another.

6.1 Introduction

SDG 6 is designed to ‘ensure the availability and sustainable management of water and sanitation for all’ (UN 2018). It defines clean, accessible water as an essential part of the world we want to live in, one that should be universally and easily accessible across the globe. As we shall see in this chapter, the anthropocentric orientation of the SDG title is later modulated by a more integrative view of some of the specific targets. However, it already shows the potential for conflict in the competition for water under conditions of scarcity. While not a central consideration in the development of SDG 6, there are intrinsic links between forests and water. Trees, as living organisms, need water to exist and thrive; as critical landscape components, they strongly influence water availability at local and continental scales. The exact nature of this influence is still a point of scientific debate, although in recent decades we have witnessed the slow emergence of a more nuanced picture of forest–water relationships. Understanding the potential impacts of SDG 6 on forests and people requires a balanced appraisal of these relationships.

The chapter first briefly summarises the current understanding of forest–water interactions in order to identify the critical SDG 6 targets for forestry. An in-depth discussion of target impacts on forest cover focuses on two areas: South America and South Asia. These two areas have diverse conditions where forests play an important role in upstream/downstream and inter-catchment interactions, where achieving SDG 6 will require active interventions. The final section takes a wider perspective to discuss the key considerations for improving SDG 6 and forestry interactions at the global scale.

6.2 Forest and Water Interactions

The traditional understanding of how forests and water interact is influenced by long-standing beliefs regarding the role of forests in the water cycle, which are not always supported by science (Calder Reference Calder2005). The current scientific understanding is much more nuanced and needs to be stated clearly in order to understand the links with the new requirements on water management emerging from SDG 6, enabling us to distinguish between positive synergies and potential misconceptions. Important initial considerations for this discussion are the big regional differences worldwide in forest cover, climate zones and land-use changes. The following summary considers both the traditional catchment-scale water balance and recent interest in the recycling of evaporated moisture at much larger, inter-catchment scales.

  1. 1. At the catchment scale, decades of research with paired catchments and process studies have shown that, relative to shorter vegetation, forest cover reduces catchment run-off at the annual scale because trees have higher rainfall interception rates and higher transpiration rates during dry periods (Andréassian Reference Andréassian2004, Bosch and Hewlett Reference Bosch and Hewlett1982, Zhang et al. Reference Zhang, Liu and Harper2017). Dry season flows are particularly likely to be reduced in forest catchments as tree roots can extract soil water from greater depths than shorter vegetation. Reductions in annual run-off for the most extreme change from 100 per cent grass cover to 100 per cent forest cover can be substantial, ranging from 15 per cent to at least 50 per cent (Fahey and Payne Reference Fahey and Payne2017, Marc and Robinson Reference Marc and Robinson2007). Run-off reduction has been found at catchment scales as large as thousands of square kilometres (Iroumé and Palacios Reference Iroumé and Palacios2013, Silveira and Alonso Reference Silveira and Alonso2009, Zhang et al. Reference Zhang, Liu and Harper2017).

  2. 2. Run-off reduction is greatest for young, growing forests. The reduction may be smaller for old mature forests with low leaf-area indices. Different tree species take up water at different rates (Huber et al. Reference Huber, Iroumé, Mohr and Frene2010).

  3. 3. In certain cases, by increasing soil infiltration and thus groundwater recharge, forests may allow a temporally more even redistribution of run-off, thus increasing dry season flows (but still with reduced annual flow) (Calder Reference Calder2005). Most evidence, however, points to a reduction in dry season flows following afforestation, although the pattern in areas with seriously degraded soils is less clear (Bruijnzeel Reference Bruijnzeel2004) and the overall effect is likely to vary with tree density (Ilstedt et al. Reference Ilstedt, Bargués Tobella and Bazié2016).

  4. 4. The special case of cloud forests, which intercept fog and cloud droplets, may possibly increase annual yields in the very specific (typically mountain) locations in which they occur (Bruijnzeel Reference Bruijnzeel2001, Reference Bruijnzeel, Mulligan and Scatena2011). However, the fog formation may itself depend in part on recycling of evaporated moisture from upwind forests.

  5. 5. At very large (subcontinental) scales, recycling of forest evapotranspiration potentially increases the downwind rainfall (Ellison et al. Reference Ellison, Morris and Locatelli2017, Sheil Reference Sheil2018, van der Ent et al. Reference van der Ent, Savenije, Schaefli and Steele-Dunne2010) and thus run-off (after any interception losses in the recipient catchment).

  6. 6. The impact of forest cover on flood peaks, as opposed to run-off, is more controversial, both because the effect on extreme flows is uncertain and because the means of quantifying the impact is disputed (see discussion in Alila and Green Reference Alila and Green2014).

  7. 7. Because of the greater evapotranspiration and consequently lower (on average) soil moisture content in forested catchments, the generally higher infiltration capacity of forest soils and the greater carbon sequestration (which aids water storage), forests can absorb more of the rain and so reduce flood peaks for given low to moderate rainfall events. This effect does not occur if the soil is already saturated, for example from a previous rain event or from soil water accumulated over a wet season (Bathurst et al. Reference Bathurst, Birkinshaw and Cisneros2011).

  8. 8. Forests may not be effective in reducing flood peaks produced by extreme (but rare) rainfall events as the above absorption effect is overwhelmed by the amount of rain (Bathurst et al. Reference Bathurst, Birkinshaw and Cisneros2011).

  9. 9. Forests can reduce the frequency with which a given flood peak occurs for all (not just low to moderate) flood sizes (Kuraś et al. Reference Kuraś, Alila and Weiler2012).

  10. 10. Forest cover often (but not always) reduces sediment yield compared with other land covers, especially those involving soil disturbance. The annual specific sediment yield in a logged catchment may exceed that in an undisturbed forested catchment by up to one order of magnitude under conditions of best management practice or two orders of magnitude in cases of severe ground disturbance or extreme events coinciding with the logged condition (Bathurst and Iroumé Reference Bathurst and Iroumé2014). However, in areas of high natural sediment yields or during certain extreme events such as tropical hurricanes, the vegetation cover may have relatively little impact on overall sediment yield (Calder Reference Calder2005).

  11. 11. By excluding other management approaches (e.g. fertiliser application) and limiting soil erosion, forests usually imply less-polluted water. Deposition of most atmospheric pollutants are generally higher to forests and, in regions of high (industrial) pollution, this has historically caused acidification of catchments and run-off, especially with coniferous forest cover (Calder Reference Calder2005). However, this threat is reducing in the advanced economies as industrial emissions are controlled and energy production moves away from coal and other fossil fuels. In certain areas (e.g. the southwest of Western Australia), the rise in the water table following the removal of forest cover has resulted in a redistribution of soluble salts, causing severe soil salinisation and loss of crop-growing capacity (Peck and Hatton Reference Peck and Hatton2003). Lowering of the water table following afforestation of grasslands has also been associated with soil salinisation (e.g. in Brazil and Hungary) (Jobbágy and Jackson Reference Jobbágy and Jackson2004, Tóth et al. Reference Tóth, Balog and Szabó2013).

  12. 12. Forest–water interactions have traditionally been studied at the river catchment scale, emphasising the impact of forest cover or its absence on downstream water users and communities. The increasing interest in the recycling of forest evapotranspiration at the subcontinental scale, though, highlights the impacts that may be felt downwind over large distances and across catchment and national boundaries (Ellison et al. Reference Ellison, Morris and Locatelli2017). Additionally, forestry activities (including forest loss) often take place on a patchwork basis, rather than uniformly across an entire catchment, especially at the larger catchment scale. Moreover, the phenomenon of deforestation and its impacts on landscape and water availability are evident at scales larger than the catchment. It is therefore necessary to consider forest–water interactions at the catchment, landscape and subcontinental scales; actions with a beneficial impact at one scale may have an adverse impact at another.

6.3. Relevance of SDG 6 to Forests and Forest People

SDG 6 is one of the new goals that emerged in 2015. Indeed, water was a notable omission from the SDG predecessors, the Millennium Development Goals (MDGs). In spite of its importance for achieving many of the MDG targets (WWAP 2009), it was hidden within MDG 7 Ensure Environmental Sustainability under the dual Target 7.C: ‘To halve the proportion of the universal population without sustainable access to clean and safe drinking water and basic sanitation by 2015’. This has important implications for SDG 6’s policy context. While most of SDG 6 is new, the goal starts with an inherited focus on the water, sanitation and hygiene (WASH) agenda, which has developed a strong momentum after nearly two decades of MDG work. The drinking-water target was considered a big success as it was met five years before the deadline, but the sanitation target was never achieved. Although the proportion of the global rural population without access to improved sanitation has declined by nearly a quarter, half of people living in rural areas, including forested areas, do not have access to these facilities (UN 2015). Given this failure and the momentum behind the WASH agenda, it seems likely that a large proportion of the resources allocated to SDG 6 will be focused on sanitation. The reality is that the impact of MDG Target 7.C on the forestry sector and related policies was minimal; the same may be expected of the WASH impact. Two exceptions are an increasing interest in (1) the role of forests – as providers of hydrological ecosystem services – in protecting clean drinking water resources (Brauman et al. Reference Brauman, Daily, Duarte and Mooney2007), and (2) the use of wastewater in forestry (FAO 2018a). In Section 6.5.2 we discuss interest in nature-based solutions, forests’ role therein and the wider role of forests in precipitation recycling.

Pointers towards an increased interaction between global water goals and forestry appear in the final MDG Report (UN 2015). It devotes attention to the 663 million people still using unimproved drinking water sources, mainly in sub-Saharan Africa but also in South Asia, and the shocking 2.4 billion still using unimproved sanitation. It highlights how 30 per cent of the planet’s land area is covered by forests that not only support 1.6 billion people but also help ‘provide additional benefits … such as clean air and water’ (UN 2015: 52) and support river catchments yielding three-quarters of the globally available freshwater. It implicitly assumes that changes in deforestation, afforestation and reforestation rates affect water resources. There are big regional differences in the way these interactions take place. South America and Africa have experienced the larger net losses of forest area, while large-scale afforestation programmes in China have offset continued rates of net loss in Southern and Southeastern Asia, all with corresponding impacts, positive or negative, on water balances. The exact nature of these processes is very important because one of the other key identified global environmental drivers is water scarcity, which affects more than 40 per cent of the global population – a figure that is projected to rise. Although the main problems are in the dry areas of Northern Africa and Western Asia, scarcity affects every continent. Major sectors that compete for water are agriculture (for irrigation, livestock and aquaculture), industries and municipalities. Agriculture, mainly through irrigation, takes nearly 70 per cent of freshwater withdrawals. Forests are not mentioned in the section about scarcity of the MDG 7 report, but their role in determining total water quantity and quality in catchments is critical.

After intense water-sector lobbying and proven interest from the public and governments in the consultations after Rio+20 (UNESCO-IHP 2014), SDG 6 has gone much further than the MDGs, with a set of completely new targets covering the whole gamut of integrated water resources management, as the water sector wanted (Table 6.1). This substantially increases the potential impact of SDG 6 on forests and forestry, as four of the new targets (6.3–6.6) are focused on water resources and not just on WASH. The drinking water and sanitation targets (6.1 and 6.2) are maintained and indeed enhanced with an ambitious ‘for all’ specification, which substantially increases their difficulty and cost. The means of implementation targets (6.A and 6.B) are neutral for the forest sector, although Target 6.B could have implications for hydrological ecosystems services involving forests. The UN SDG 6 synthesis report (UN 2018) reinforces the message that water management is critical. Water scarcity, flooding and quality are identified as the key determinants in social and economic development, and water efficiency is identified as the main factor to balance growing competing demands. The new SDG 6 targets incorporate all these aspects and, consequently, define the areas where SDG 6 implementation potentially impacts upon forests significantly.

Table 6.1 SDG 6 targets and monitoring indicators for Targets 6.36.6

6.1 By 2030, achieve universal and equitable access to safe and affordable drinking water for all
6.2 By 2030, achieve access to adequate and equitable sanitation and hygiene for all and end open defecation, paying special attention to the needs of women and girls and those in vulnerable situations

6.3 By 2030, improve water quality by reducing pollution, eliminating dumping and minimizing release of hazardous chemicals and materials, halving the proportion of untreated wastewater and substantially increasing recycling and safe reuse globally

Indicators: 6.3.1 Proportion of wastewater safely treated

6.3.2 Proportion of bodies of water with good ambient water quality

6.4 By 2030, substantially increase water-use efficiency across all sectors and ensure sustainable withdrawals and supply of freshwater to address water scarcity and substantially reduce the number of people suffering from water scarcity

Indicators: 6.4.1 Change in water-use efficiency over time

6.4.2 Level of water stress: freshwater withdrawal as a proportion of available freshwater resources

6.5 By 2030, implement integrated water resources management at all levels, including through transboundary cooperation as appropriate

Indicators: 6.5.1 Degree of integrated water resources management implementation (0–100)

6.5.2 Proportion of transboundary basin area with an operational arrangement for water cooperation

6.6 By 2020, protect and restore water-related ecosystems, including mountains, forests, wetlands, rivers, aquifers and lakes

Indicator: 6.6.1 Change in the extent of water-related ecosystems over time

6.A By 2030, expand international cooperation and capacity-building support to developing countries in water- and sanitation-related activities and programmes, including water harvesting, desalination, water efficiency, wastewater treatment, recycling and reuse technologies
6.B Support and strengthen the participation of local communities in improving water and sanitation management

(orange = WASH targets; yellow = targets and indicators with potential forest impacts; white background = means of implementation targets)

Progress towards achieving each SDG 6 target is quantified by at least one indicator (UN Water 2018a). Section 6.4 assesses target impacts on forests through the actions that will be needed to ensure a positive direction for the respective indicator(s). Indicators 6.3.1–6.6.1 are the main focus of the analysis. Indicators 6.1.1 and 6.2.1 are the proportion of the population using, respectively, safely managed drinking water and sanitation services.

6.4 SDG 6 and Forests: Key Links

This section examines the potential impacts of SDG 6 on forests (summarised in Table 6.2).

Table 6.2 Potential impacts of SDG 6 indicators on forests

IndicatorResponse for favourable indicator score
6.1.1 Proportion of population using safely managed drinking water servicesMaintain forest cover to ensure good water quality in water supply catchments.
Establish forested riparian buffer strips to maintain stream water quality.
6.2.1 Proportion of population using safely managed sanitation services, including a hand-washing facility with soap and waterNo direct link but target generally favourable for forest people.
6.3.1 Proportion of wastewater safely treatedEncourage agroforestry schemes using treated wastewater.
Maintain forest cover for treating wastewater (e.g. in schemes for induced precipitation recycling).
6.3.2 Proportion of bodies of water with good ambient water qualityMaintain or increase forest cover to enhance water quality.
Change plantation tree species to enhance water quality and quantity.
6.4.1 Change in water-use efficiency over timeRequire increased water efficiency from forests as forestry is combined with (relatively inefficient) agriculture in allocating available water between economic activities.
Change plantation tree species, density and location to improve water-use efficiency.
6.4.2 Level of water stress: freshwater withdrawal as a proportion of available freshwater resourcesRestrict establishment and continuation of plantation forest in water-limited areas (e.g. semi-arid regions) to maximise water availability.
Maintain forest cover in upwind areas to safeguard downwind water resources dependent on recycled evapotranspiration.
6.5.1 Degree of integrated water resources management implementation (0–100)Integrate forest management with water resources management.
Change plantation tree species, plantation characteristics and riparian buffer strips to optimise water availability and quality.
6.5.2 Proportion of transboundary basin area with an operational arrangement for water cooperationIntegrated consideration of forest management, including downstream impacts (within catchment) and downwind impacts (between catchments).
6.6.1 Change in the extent of water-related ecosystems over timeReforest agricultural land, replace exotic tree plantations with native forests and implement other scenarios to maintain water availability and quality, with potential impacts on forest people.

6.4.1 Access to Safe and Affordable Drinking Water and Adequate and Equitable Sanitation and Hygiene – Targets 6.1 and 6.2

As noted in Section 6.3, Target 6.1 is somewhat neutral regarding the forest sector. Forests do not, of themselves, provide safe drinking water or sanitation services. Nevertheless, to the extent that stream waters in forested catchments tend to be of higher quality than in agricultural or urban environments, the treatment costs to bring them to a safe potable level may be lower, with a beneficial effect on affordability. It is common to find catchments maintained with a forest cover to form a source of clean water for a nearby city (e.g. Valdivia, Chile, receives water from a 12.7 km2 catchment hosting evergreen native forest). Also, direct extraction of drinking water from streams without treatment is also generally safer in forested catchments than elsewhere (e.g. important for Indigenous populations of tropical forests). The performance of Indicator 6.1.1 (Proportion of population using safely managed drinking water services) could therefore be enhanced by a greater forest cover in water supply catchments. In some regions, forest cover is increasing through natural regeneration following abandonment of agricultural land. In other cases it may be worth deliberately afforesting catchments to provide purer water for water treatment plants, as the cost of treating lower-quality water in the absence of forest cover can be high (hundreds of thousands to millions of US dollars per year for individual cities; Ashagre et al. Reference Ashagre, Platts and Njana2018). That cost would have to be compared with the costs of afforestation (including the potential removal of people from the land and the loss of agriculture). Reduction in run-off, and thus water availability, resulting from the afforestation would also have to be considered (e.g. Target 6.4). A more feasible and cheaper option may be the introduction of forested buffer strips along riparian zones, to reduce or interrupt nutrient fluxes to streams in agricultural catchments and sediment fluxes from both agricultural catchments and forested catchments undergoing logging. In the absence of other pressures, Indicator 6.1.1 is likely to favour maintaining existing forest covers. Given the multiple pressures on land resources, however, it would not be surprising if the forests’ (high) worth to drinking-water quality was simply ignored, leaving the successful achievement of Target 6.1 increasingly dependent on artificial water treatment. The target would then be irrelevant to forests. Target 6.2, with its emphasis on sanitation and hygiene for all, should have a positive impact on forest people – that is, those who live in forests and whose lives and livelihoods depend directly on the forest environment and forest resources. Difficulties of accessibility, though, are likely to mean that forest people in remote areas will be among the last to benefit from this target (although perhaps being among those least in need of it).

6.4.2 Improving Water Quality – Target 6.3

Indicator 6.3.1 (Proportion of wastewater safely treated) is not closely linked to forests. However, to the extent that there is an interest in using treated wastewater for forestry, this indicator may drive an increase in, for example, agroforestry schemes. Forests have themselves been proposed as treatment areas for wastewater as part of wider schemes for induced precipitation recycling (Layton and Ellison Reference Layton and Ellison2016). Indicator 6.3.2 (Proportion of bodies of water with good ambient water quality) is more relevant in view of the potential for land use to affect water quality in rivers, reservoirs, estuaries and downstream wetlands. For example, in streams in native forests in Chile, nitrate (NO3-N) and ammonium concentrations are very low and nitrogen (N) export is very low (0.2–3.5 kg N ha-1 yr-1) (Perakis and Hedin Reference Perakis and Hedin2001, Reference Perakis and Hedin2002). The conversion of native forests to other land uses may therefore be expected to lead to increased NO3-N and total N export. Conversion of native forest to pasture in southern Chile is associated with increased N fluxes and increased dominance of NO3-N (exports up to 11 kg ha-1 yr-1), although some of this increase may be attributable to pasture fertilisation (Oyarzún and Huber Reference Oyarzún and Huber2003). Conversely, afforestation may change soil pH and alter nutrient cycles (Hong et al. Reference Hong, Piao and Chen2018). Nevertheless, because fertiliser use in plantation forestry – in terms of total use – involves a lower application frequency and smaller land areas compared with agricultural systems (May et al. Reference May, Smethurst and Carlyle2009), the conversion of crop or pastureland to plantations (or even reverting to natural forest) is expected to improve water quality.

In most cases, logging of planted forests may produce elevated sediment export, mainly because of mechanised site preparation, road building and clear-cutting operations in steep terrain, rather than exposure of soil to rainfall (Bathurst and Iroumé Reference Bathurst and Iroumé2014). Research in forest plantations in central Chile found that forest roads produce more sediment than hill slopes; after clear-cutting, the relative contributions increased from 16 per cent to 25 per cent for hill slopes and from 37 per cent to 45 per cent from forest roads (Schuller et al. Reference Schuller, Walling and Iroumé2013). Sediment delivery to streams increases if logging operations take place in rainy periods (with adverse impacts on drinking water and aquatic habitats), but the application of contemporary best management practices, which include guidelines for logging during dry periods, can limit logging-related sedimentation (Bathurst and Iroumé Reference Bathurst and Iroumé2014). Although forest certification has enhanced the adoption of best management practices in Chile, forestry operations are still associated with increased sediment transport and decreases in water quality relative to unmanaged forests.

Because of forests’ generally positive impact on water quality, Indicator 6.3.2 favours maintaining forest cover and increasing cover in protected or degraded catchments. Specifically, achieving good indicator scores for plantation forests will require careful consideration of tree species and the development and implementation of best management practices.

6.4.3 Water Efficiency and Improved Availability – Target 6.4

Indicator 6.4.1 (Change in water-use efficiency over time) tracks the value added (in US dollars) per volume of water withdrawn (cubic metres), by a given economic activity over time (UN Water 2018a). The UN International Standard Industrial Classification of All Economic Activities, Revision 4 code combines forestry with agriculture and fishing. This means that forestry as an economic activity will be considered jointly with agriculture when comparing water use with other sectors. It is already acknowledged that irrigation, as the largest consumer of water by volume, should be one of the big targets for water efficiency (HLPW 2018). There will therefore be increased attention to the efficient use of water in the forestry sector, which may eventually constrain the establishment and continued presence of plantation forests in the water-stressed areas highlighted by Indicator 6.4.2 (Level of water stress: freshwater withdrawal as a proportion of available freshwater resources). This indicator is demand-driven and measures the ratio between withdrawals and the difference between total renewable water resources and the environmental flows (Vanham et al. Reference Vanham, Hoekstra and Wada2018). Strictly, it considers only blue water: the liquid water in rivers, lakes, wetlands and aquifers. However, the amount of blue water is determined by the upstream flows of green water – rainwater held in the unsaturated zone of the soil and available to plants – which is determined by terrestrial ecosystem functions or natural land use (e.g. forests or natural grasslands) and by consumptive water use in rain-fed agriculture and forest plantations. Therefore, analyses of water-stressed environments may lead to closer examinations of the consumptive use of water by forests.

In terms of biomass production per litre of water, trees are considered efficient users of water. Nevertheless, Soto-Schönherr and Iroumé (Reference Soto-Schönherr and Iroumé2014) found in Chile that water-use efficiency (i.e. kilograms of biomass produced per unit of water consumed) differs only a little between forests and grasslands: forests produce 0.1–4 kg of biomass per cubic metre of water, while grasslands produce 0.5–1.3 kg. However, because trees use more water than shorter vegetation, there is a central inconsistency (at least at the catchment scale) between the aims of maintaining forest cover (desirable for many reasons, including lower soil erosion and higher water quality) and of increasing water availability (which implies reducing forest cover). This is less concerning in high-rainfall areas (where there is enough water for all activities) but could be critical in semi-arid areas. This means that forestry as an economic activity will be compared directly with agriculture and other activities when deciding on use of limited water resources. Replacing forest by agriculture could increase annual run-off (and food supply), but at the expense of the forest ecosystem and timber supply. For example, replacement of natural vegetation with agricultural cover in a 175 360 km2 catchment in South America produced a significant increase in annual mean discharge and high-flow season discharges because of reduced infiltration and evapotranspiration rates (Costa et al. Reference Costa, Botta and Cardille2003). Conversion of forest cover may ultimately lead to destruction of the land resource itself (Contreras et al. Reference Contreras, Santoni and Jobbágy2013). Thinning of forests considered unnaturally overgrown as a result of fire-suppression programmes has been proposed to increase water supply, e.g. in North America (Poulos Reference Poulos2018), but this may ignore the many other changes produced by forest management (Jones et al. Reference Jones, Achterman and Augustine2009, NRC 2008). For example, forests play important roles in regulating the world’s temperatures and freshwater flows, storing carbon and providing a broad range of important but less recognised benefits (Ellison et al. Reference Ellison, Morris and Locatelli2017). At the subcontinental scale, replacement of forests by shorter vegetation could imply less rainfall in downwind regions (Creed and van Noordwijk Reference Creed and van Noordwijk2018) and possibly therefore less run-off, although the magnitude of this effect remains to be quantified.

Overall, forest plantations with fast-growing species use more water than native forests, although many of the comparisons are limited to old-growth native forests versus young plantations (Soto-Schönherr and Iroumé Reference Soto-Schönherr and Iroumé2016). Results from southern Chile, for a wide range of latitudes and forest compositions and ages, showed that annual interception accounts for approximately 21 per cent of incoming precipitation in the mean, albeit with some margin of variation (Soto-Schönherr and Iroumé Reference Soto-Schönherr and Iroumé2016). Within the range of variation, broad-leaved forests (including native broad-leaved and eucalyptus forests) generally exhibit higher interception losses than conifers. Indicative of the level of uncertainty, Huber et al. (Reference Huber, Iroumé, Mohr and Frene2010) found that interception is lower, and water use is higher, in eucalyptus compared with pine plantations in southern Chile. Because of the relatively limited difference in canopy interception loss between native forests and forest plantations (Huber and Iroumé Reference Huber and Iroumé2001, Soto-Schönherr and Iroumé Reference Soto-Schönherr and Iroumé2016), the observed differences in water yield between the two must be explained, at least in part, by different transpiration losses.

Despite the above, forest plantations may not use more water than native forests at all stages of the forest rotation. As expected, water use is highest (and yield lowest) in the late stages of plantation growth, especially in short-rotation plantations with a high tree density, but water yield (especially summer water yield) increases just after clear-cutting, in the early phases of replanting (Iroumé et al. Reference Iroumé, Huber and Schulz2005, Reference Iroumé, Mayen and Huber2006). Again, variations between plantation species may exist (e.g. pine versus eucalyptus). Thus, water consumption by forests could be moderated by a small amount through careful choice of tree species (with an eye towards suitability to future climates), maintaining a mix of old and new growth (i.e. avoiding large-scale plantation of new growth), regulating tree density and choosing plantation location carefully, possibly implying longer growth periods or reduced timber yield. Nevertheless, such moderation is likely to be small compared with the effect of forest removal. Overall, the demands of Target 6.4 are likely to be inimical towards forest cover in many parts of the world.

6.4.4 Integrated Water Resources Management – Target 6.5

Integrated water resources management (IWRM) is defined as ‘a process which promotes the coordinated development and management of water, land and related resources in order to maximise economic and social welfare in an equitable manner without compromising the sustainability of vital ecosystems’ (Global Water Partnership 2017). It acknowledges the interconnected nature of hydrological resources and the interdependence of different water uses. Within the wider requirements of the definition, IWRM implementation implies the integrated management of water supply, water quality, flood management, navigation, hydroelectric power generation and other water provisions and services within a river basin. Within this balancing act, forest cover reduces water supply relative to other vegetation covers (at the annual scale) but has the potential to improve water quality. From points 8 to 10 in Section 6.2 it can be concluded that forest cover could probably be reduced without necessarily increasing damaging flood magnitudes, but flood frequencies might increase, as would soil erosion. These points refer to the catchment scale. At the subcontinental scale, forest evapotranspiration is not lost from the system but may be recycled as precipitation downwind. Water resources management needs to be integrated with forest management, an end likely encouraged by Indicator 6.5.1 (Degree of integrated water resources management implementation). Such integration is most required in regions where there are multiple and conflicting demands for water, where water supplies are restricted and forests account for significant water use (e.g. semi-arid regions) and where soil erosion is a significant problem (e.g. semi-arid regions, degraded lands and areas of unregulated agricultural expansion). The exact impact of Indicator 6.5.1 on forest cover will vary from basin to basin depending on economic, social, political and other circumstances. It seems more likely, though, that IWRM is implemented as a function of whatever level of forest cover happens to exist, and therefore reacts to rather than drives forest cover change.

In South America conversion of forest to agriculture is the major reason for changes in water availability to rivers and streams (Jones et al. Reference Jones, Almeida and Cisneros2017). The concept of virtual water (Yang and Zehnder Reference Yang and Zehnder2007) assesses water-use efficiency based on water used to grow products traded globally. From 1986 to 2007, South America increased its annual use of water from 42 km3 to 178 km3 and became the continent using the greatest amount of water in food products traded globally, with significant increases in soy exports to China – which in turn has contributed to deforestation in Amazonia (Dalin et al. Reference Dalin, Konar, Hanasaki, Rinaldo and Rodriguez-Iturbe2012).

In the Federal District of Brazil, river basins with substantial expansion of agriculture since the end of the 1970s show a dramatic decrease of base flow discharge by 40–70 per cent – presumably the effect of irrigation extractions more than compensating for the increase in run-off otherwise expected from reduced forest evapotranspiration. Additionally, the run-off ratio is significantly positively related to the cover of natural vegetation (Lorz et al. Reference Lorz, Abbt-Braun and Bakker2012). In south-central Chile, the run-off ratios in four large catchments were positively related to the area of native forest and negatively related to the area of eucalyptus and pine plantations (Lara et al. Reference Lara, Little and Urrutia2009).

Careful choice of tree species and plantation characteristics could moderate water consumption by forests. Reducing the area of forest plantations can potentially increase water availability at the catchment scale, as might replacing exotic fast-growing trees with native forest species, although it has yet to be proven that this would allow adequate timber yields to be produced with less water use. Native forest riparian buffers may increase water yield and improve water quality in forest plantations of eucalyptus in south-central Chile (Little et al. Reference Little, Cuevas, Lara, Pino and Schoenholtz2015) and along rivers in degraded native forest in southeast Brazil (de Souza et al. Reference de Souza, Fonseca, Liborio and Tanaka2013). Forest thinning (Poulos Reference Poulos2018) should be approached with caution: thinned plantations may initially increase water yield (Forrester et al. Reference Forrester, Collopy, Beadle, Warren and Baker2012), but subsequent forest growth might take up the additional water, depending on the timing and degree of thinning (Perry and Jones Reference Perry and Jones2017).

At the international level, Indicator 6.5.2 (Proportion of transboundary basin area with an operational arrangement for water cooperation) may drive a more integrated consideration of the forest environment, especially where a downstream or downwind state feels adversely affected by the forestry activities of an upstream or upwind state. At the subcontinental scales typical of many politically sensitive transboundary basins, the downstream impacts of upstream forestry activities may not always be significant. For example, there is no clear evidence for the so-called Himalayan environmental degradation theory, which proposes that loss of forest cover caused by a rapidly growing population in the Himalayan headwaters of the Ganges and Brahmaputra Rivers increases soil erosion and flood run-off, thereby generating increased flooding and siltation in the delta regions of Bangladesh (Hofer Reference Hofer1993). Downwind impacts at subcontinental scales are increasingly thought to be important but have yet to be proven conclusively (Creed and van Noordwijk Reference Creed and van Noordwijk2018). Large amounts of moisture from evapotranspiration may be recycled within Amazonia and transferred to other parts of South America. However, the extent to which forest conversion has affected this precipitation recycling so far is yet to be clearly quantified (Bagley et al. Reference Bagley, Desai, Harding, Snyder and Foley2014, Khanna et al. Reference Khanna, Medvigy, Fueglistaler and Walko2017, Spera et al. Reference Spera, Galford, Coe, Macedo and Mustard2016, Swann et al. Reference Swann, Longo, Knox, Lee and Moorcroft2015). The impact of Target 6.5 is most likely to be a more integrated consideration of forest management, especially with respect to water resources management, both within and among river basins.

6.4.5 Protecting and Restoring Water-Related Ecosystems – Target 6.6

Indicator 6.6.1 (Change in the extent of water-related ecosystems over time) will drive careful consideration of the relationship between forest cover and the health and sustainability of water-related ecosystems. Although the title of Target 6.6 includes forests along with mountains, wetlands, rivers, aquifers and lakes, Indicator 6.6.1 considers only mangroves. The absence of other types of forests severely limits this indicator’s degree of protection.

Despite the restricted nature of the indicator, forest-related water ecosystems services form an important underlying concept linked to the essence of Target 6.6. They are indeed one of the most proffered links between SDG 6 and forests, but they are not always properly understood and are difficult to quantify. For instance, not all forested areas safeguard water quality: rapid and aggressive afforestation and reforestation with exotic species reduces water availability, affecting its quality, especially in dry seasons (Filoso et al. Reference Filoso, Bezerra, Weiss and Palmer2017). Achieving good indicator scores requires maintenance of water flows – and of good water quality – to wetlands. This could imply reforesting agricultural areas, replacing plantations of exotic tree species and monocultures with a wider range of native trees (which may be slower growing), removing existing plantations or avoiding new plantations (e.g. in peatlands, páramo soils or semi-arid regions) and other scenarios. Such land management could have adverse consequences for livelihoods based on the existing agricultural and plantation activity (and for the production of the associated crops) but might open new employment prospects in forestry activities. Also, there is a high potential for payments for ecosystem services if those services are clearly proven. In the Hindu Kush Himalaya region, research is attempting to show the tangible value of water-related ecosystem services; for example, purification of the downstream water supply via upstream forests is an important ecosystem function that payments for ecosystem services schemes have attempted to quantify and that can contribute to achieving Target 6.3 by natural means (Ashagre et al. Reference Ashagre, Platts and Njana2018). However, there is still a gap in our understanding of how individual attributes (such as changes in land-use patterns) impact ecosystem service flows, including water (Polasky et al. Reference Polasky, Nelson, Pennington and Johnson2011, Nelson et al. Reference Nelson, Kareiva and Ruckelshaus2013, Su and Fu Reference Su and Fu2013). In particular, it is difficult to correlate change in a land unit with change in the volume of ecosystem services that this unit provides (Bhatta et al. Reference Bhatta, Khadgi and Rai2017).

Despite these uncertainties, payments are already being made to promote ecosystem services. Recently, the Chilean government, acting according to the UN Framework Convention on Climate Change (UNFCCC), gave a commitment to afforest (mainly with native tree species) 100 000 ha of degraded soils as a contribution to reducing greenhouse gases (CONAF 2016). To this is added some 470 000 ha that were burnt during the 2016–2017 (southern) summer season. Of this, the government will finance the afforestation of 100 000 ha on lands belonging to small- and medium-size owners, while the remaining burnt lands owned by larger forest companies are already being afforested. The aims of these afforestations are mainly to restore and improve the ecosystem services of the degraded areas, except for the afforestation of lands owned by larger private forest companies whose purpose remains timber production. Not all those forested areas would safeguard water quantity; potentially, there could be resistance to forestry plantations in water-stressed regions, as highlighted by Indicator 6.4.2.

In conclusion, SDG 6 seems unlikely to exert a major influence on forest cover, and indeed is unlikely to be pursued with forests at the forefront of consideration (Table 6.2). Possible exceptions are that Target 6.4 may restrict the spread of new plantations in semi-arid areas and Target 6.5 may drive a more integrated view of catchments and their management. Plantations may be developed with more careful consideration of tree species and plantation characteristics. It seems much more likely, however, that native forest cover in much of the world will continue to decline in the face of pressures greater than SDG 6: (1) to convert forest for food production, driven by population growth and increasing aspirations for living standards worldwide; and (2) to exploit timber and other forest resources, driven first by those seeking a profit but ultimately responding to individual demand globally, with little consideration for the resulting impacts. The decline is exacerbated by the inability or unwillingness of governments in many countries to control such developments, and possibly by climate change reducing or shifting the areas of the world suitable for sustaining the current forests (Guardian 2019, WWF 2019). The extent of monoculture plantations, on the other hand, could increase or decrease: demand for plantation products (e.g. palm oil and timber) is likely to increase, but water efficiency considerations may curtail the spread of plantations in water-stressed areas.

6.5 Future Policy Considerations

6.5.1 Contextual Factors for SDG 6: The Hindu Kush Himalayas

Trying to understand the real impacts that SDG 6 may have on forests and forest people requires a careful evaluation of the context of water–forest interactions, in particular physical and social settings and the interactions with other SDGs. While context is always affected by local conditions, some situations do recur. The Hindu Kush Himalayas case illustrates some of the contextual factors that must be considered in implementing SDG 6 and highlights the upstream/downstream relationships, inherent where forested mountain areas feed major river systems, which can be found on all continents.

The Hindu Kush Himalayas harbour major river systems providing services, particularly in the form of recharge, to a mountain population of 240 million and a downstream population of 1.9 billion. Indirectly, 3 billion people are dependent on numerous ecosystem services, including climate and hydrological services provided at regional and global scales, and harvested commodities traded at multiple economic scales (Kotru et al. Reference Kotru, Rathore and Pradhan2015). The observed overall increase in forest cover in India does not mean that forest degradation is controlled. An alarming rate of deforestation in parts of the Himalayas, primarily for agricultural land and fuel supply, threatens the sustained flow of forest ecosystem services. As is generally the case in South Asia, multiple sectors and actors influence forests and forest management; it is not only through forest management that the forest–water relationship can be improved for sustained water yield.

Multiple water-related objectives across a portfolio of SDGs present new challenges for policymakers and managers of forests and landscapes with partial tree cover. Hence, SDG 6 cannot be seen in isolation from other key challenges in the Himalayas, such as SDGs 1 (No Poverty), 2 (Zero Hunger) and 5 (Gender Equality). Thus, investments (e.g. in mass tourism) made upstream for addressing other SDGs are not necessarily environmentally friendly or complemented by good governance, making it potentially more difficult to achieve the SDG 6 targets (6.1, 6.3, 6.4 and 6.6). On the other hand, the policies, practices and investments necessary to achieve SDG 6 may not be coordinated with those for other SDGs, so positive outcomes for people are not ensured (Singh and Kotru Reference Singh and Kotru2018). The transboundary nature of hydrological resources – overlaying local, regional and national boundaries – make the challenges to safe water access more complex. New institutional responses are needed to tackle multiple water-related objectives across the full portfolio of SDGs, taking a multiple benefits approach (Creed and van Noordwijk Reference Creed and van Noordwijk2018). A distinction may be made between a first group of SDGs (SDGs 1, 2, 6, 7) implying an increased demand for clean, reliably flowing water, and a second group of SDGs (5, 10, 12, 16) that stresses a change in power-sharing that allows multi-stakeholder involvement, thus increasing the need for transparency and equity in decision-making.

Several socio-economic and governance realities challenge forest regimes in fulfilling their socio-ecological role (as envisaged under SDG 6) in the Hindu Kush Himalayas (Kotru et al. Reference Kotru, Sharma, Sharma and Hofer2017):

  • poverty and inequity are still prevalent in South Asia, a water-deficit area;

  • institutional capacities and existing policies are inadequate to meet the future challenge of forest management for sustained water yields;

  • research on the forest–water relationship is essentially very limited, with no long-term monitoring data or studies available;

  • there are very limited cross-sector policy interfaces (e.g. water policy and forest policy interface) that focus on a forest or landscape approach aimed at sustaining water services;

  • sustainable forest management is seriously disadvantaged by a lack of proactive management, itself arising from policy deficits;

  • data deficits and a lack of harmonised methodologies and data sharing mean that the planning and application of conservation and development strategies contributing to SDG 6 have only a limited foundation on firm data.

Future progress towards achieving Targets 6.36.6 in the Hindu Kush Himalayas will require improved upstream–downstream integration, improved transboundary cooperation and greater coordination and simultaneous progress in the implementation of different SDGs: for example, SDGs 1, 2 and 5 (already mentioned) and SDGs 13 (Climate Action), 15 (Life on Land) and 17 (Partnerships for the Goals). Adoption of a landscape approach would allow stakeholder priority interventions to be matched with public and private investments but, equally, there is a need for an improved understanding of the role of forests in influencing ecosystems services at the larger landscape scale. Greater efforts are required to make the communities struggling on the frontline of sustainable forest management more climate resilient.

6.5.2 Implementation of SDG 6

The final impact of SDG 6 on forests and forest people will be determined by the extent of its implementation. There are four important considerations here: finances, institutions, data and other SDGs. First, implementation costs are increasing: the estimated cost of achieving the WASH targets is USD 1.7 trillion (Hutton and Varughese Reference Hutton and Varughese2016). While there are no reliable estimates of the whole cost of achieving SDG 6, it is clear that the required threefold increase for Targets 6.1 and 6.2 alone indicates a huge increase in water targets expenditure. As aid is decreasing, it is not at all clear where this money will come from. The UN calls for more technology transfer and new financing mechanisms, with some based on the recognition of the economic value of water and freshwater ecosystems (UN 2018). Forests may eventually benefit from the growing interest in nature-based solutions, which use or mimic natural processes to enhance water availability and water quality and to reduce risks associated with water-related disasters and climate change. The UN High Level Panel on Water specifically mentions that natural capital solutions, including the ‘water-retaining abilities of forest’, can be used at a fraction of the cost of engineering solutions (HLPW 2018). It labels forests as ‘natural infrastructure’ required to assure future supplies of water, calling for a better alignment of incentives to recognise the value of these services. It is of the utmost importance that natural capital solutions recognise the nuanced role of forests currently accepted as best practice and take into account local conditions. They should be particularly considered in the context of deforestation and forest degradation while recognising the need to understand water quantity effects at catchment, regional and continental scales. It is important to acknowledge that not all water-poor locations have forests to use as improvement tools.

Second, the success of SDG 6 depends on the existence of national and global institutions able and willing to implement the goal. While the WASH sector has spent nearly 20 years trying to achieve global targets, the level of institutional readiness for the new water resources targets is frequently low or non-existent at the country level. Even with the apparently successful MDG 7.C drinking water target, 53 countries were seriously off-target and 19 could not produce data. Good water governance depends on strong formal and informal institutions and the accompanying human resources. There is an acute lack of capacity across most developing countries, particularly in sub-Saharan Africa and South and Southeast Asia (UN 2018). With low institutional capacity, we can expect a slow articulation of the new targets within SDG 6 and, subsequently, low impact on the forest sector. However, since the creation of UN Water in 2003 as a focal point for coordinating efforts of UN entities and international organisations working on water and sanitation issues, the alignment of global water initiatives has increased (UN Water 2018b). Eventually this will lead to actions on the ground. The existence of SDG 6 in itself is a clear proof of the strength of these efforts. The HLPW (High Level Panel on Water 2018) has identified a number of initiatives especially relevant for states trying to implement SDG 6: the World Water Data Initiative; the OECD Water Governance Initiative; the Delta Coalition; High-level Experts and Leaders Panel on Water and Disasters, including an Alliance of Alliances on disaster risk-reduction researches; the initiative on Financing Water Infrastructure convened by the OECD; and the Water Innovation Engine. Whether these will accelerate SDG 6 implementation is yet to be seen, but they may support natural infrastructure projects with a role for forests.

The third consideration is the challenge of having enough good-quality data for monitoring SDG 6. It took a serious global effort from 1990 onwards to develop the WHO/UNICEF Joint Monitoring Programme, now the custodian of global WASH data for Targets 6.1 and 6.2. The situation is more complicated with the other targets as many countries lack the financial, institutional and human resources to acquire and analyse the required data. Fewer than half of UN member states have comparable data available on progress towards meeting the SDG 6 targets (UN 2018). This is important because countries will focus on being able to report to the Integrated Monitoring Initiative (UN Water 2018a). Accordingly, the factors monitored for each target are likely to become the focus of public policy. It is therefore important to understand how forests relate to this monitoring programme.

The final consideration is the dynamic interdependence between SDG 6 and the other SDGs (UN Water 2018c). The majority of these interlinkages are positive and mutually reinforcing. Since the MDG programme, the WASH targets have been identified as critical to: reducing poverty (SDG 1), malnutrition (SDG 2) and diseases (SDG 3); supporting education (SDG 4); and addressing gender (SDG 5) and other inequalities (SDG 10). Moreover, SDG 6 highlights how water of sufficient quality and quantity is required for food production (Target 2.4) and sustainable consumption and production (SDG 12). However, there are some targets – such as doubled agricultural productivity (Target 2.3), energy for all (Target 7.1) and sustained economic growth (Target 8.1) – that potentially could impact negatively on water resources and water ecosystems and, as such, on forests and forest people. IWRM (Target 6.5) is the appropriate framework to balance all these competing needs, for water and forests.

6.5.3 Integration of SDG 6 and Forests

The discussion of the contextual challenges in South Asia clearly shows both the difficulty and the necessity of aligning SDG 6 and forest policies. For this alignment to succeed in an IWRM framework, we need to follow a landscape approach at all levels. As larger forms of vegetation, trees use great amounts of water to produce biomass and for the process of evapotranspiration, more so than many other vegetation types, including crops and grasses. However, when considering Target 6.4 on increasing water-use efficiency and ensuring sustainable withdrawals and supply of freshwater and how it may impact forests and forest management, several issues need to be considered.

Firstly, most forests or tree-based landscapes are naturally occurring, rain-fed systems. Globally, only 7 per cent of forests are planted forests, predominantly found in temperate zones (FAO 2015). Moreover, most of these planted forests are native species: only 20 per cent of planted forests – 1.4 per cent of forests globally – are exotic, and these are located mainly in the southern hemisphere (FAO 2015). It is assumed that natural forests will not be removed for the purposes of achieving Target 6.4 as they provide a wealth of other goods and services, including water-related ecosystem services. Consequently, discussion of water-use efficiency will be limited to planted forests, despite their representing only a small proportion of global forests.

Trees are highly resilient and adaptive organisms that optimise their water use. In other words, they drastically reduce their water consumption in periods of drought and use what they can when water is available (Chaves et al. Reference Chaves, Pereira and Maroco2002). This means that during periods without rain trees can use water stored in the soil; they generally have higher annual rates of water use than shallow-rooted, annual cropping and pasture systems. In high-rainfall areas (> 1500 mm per annum), planted forests can use up to 200 mm more water than pastures, but only if the water use is not energy limited. In low rainfall areas (< 600 mm per annum), forest plantations use an amount of water similar to annual crops and pastures. In intermediate rainfall areas, planted forests potentially use more water than annual crops and pastures. If this is in conflict with other demands for water, policies are required to regulate allocation of water to plantations among other uses. Policy instruments to regulate plantation water can be direct (e.g. a moratorium on land concessions) or indirect (e.g. a market for allocable water). For example, South Africa, Australia and India have implemented policies to regulate or limit plantation establishment (Brown et al. Reference Brown, Zhang, McMahon, Western and Vertessy2005, Dye and Versfeld Reference Dye and Versfeld2007, Farley et al. Reference Farley, Jobbágy and Jackson2005, van Dijk and Keenan Reference van Dijk and Keenan2007, Whitehead and Beadle Reference Whitehead and Beadle2004).

Even if trees are able to optimise their water use, it is important to note that management can be improved in order to further optimise water-use efficiency – including tailoring species selection, as well as thinning and harvesting techniques – to the environmental conditions such as slope, soil type and condition. More importantly, as planted forests are managed at the stand scale and water is managed at a catchment or basin scale, it is critical when planning to look at planted forests, and even tree-based systems more broadly, at the landscape level, taking into consideration the mosaic of land uses and their effects on water. This requires a cross-sectoral approach to land and water planning and management.

Integrated planning and management may require reframing our approach, taking into account integrated solutions such as agroforestry and the use of recycled wastewater in planted forests. Studies show that agroforestry increases water-use efficiency (Bai et al. Reference Bai, Sun and Zheng2016, Droppelmann et al. Reference Droppelmann, Lehmann, Ephrath and Berliner2000). The recycling of treated wastewater for planted forests can reduce competition for water use (particularly in semi-arid and arid areas where water is scarce), reduce the costs associated with water treatment and reduce downstream contamination (FAO 2018a). Planted forests irrigated with treated wastewater in turn improve soil water-storage capacity, reduce soil degradation and erosion, combat desertification in arid areas and provide essential goods that support livelihoods, such as timber, pulpwood and fuelwood (FAO 2018a). According to FAO’s Aquastat database (FAO 2018b), only 52 per cent of the municipal wastewater produced globally is recycled, so there is ample opportunity to explore such options. Egypt, Jordan, Mexico and Spain, among others, are exploring the use of treated wastewater for agroforestry and planted forests. In Jacksonville, North Carolina, USA, upstream forests are being irrigated with treated wastewater, with the forests acting as the final stage of the filtering process and returning water back into the catchment for use downstream (Tew Reference Tew2016).

Much can be gained from a deeper integration of SDG 6 and forest policies. However, this integration must be guided by a shared understanding of the complex relationships between water and forests and their impacts on both forest people and the communities downstream, and possibly downwind.

Acknowledgements

The authors thank the internal and external reviewers, all anonymous, for suggestions that have helped to improve the chapter.

Footnotes

* Lead authors.

References

Alila, Y. and Green, K. C. 2014. Reply to comment by Bathurst on ‘A paradigm shift in understanding and quantifying the effects of forest harvesting on floods in snow environments’. Water Resources Research 50:2759–64. doi:10.1002/2013WR014334.Google Scholar
Andréassian, V. 2004. Waters and forests: From historical controversy to scientific debate. Journal of Hydrology 291:127.Google Scholar
Ashagre, B. B., Platts, P. J., Njana, M. et al. 2018. Integrated modelling for economic valuation of the role of forests and woodlands in drinking water provision to two African cities. Ecosystem Services 32:5061.Google Scholar
Bagley, J. E., Desai, A. R., Harding, K. J., Snyder, P. K. and Foley, J. A. 2014. Drought and deforestation: Has land cover change influenced recent precipitation extremes in the Amazon? Journal of Climate 27(1):345–61.Google Scholar
Bai, W., Sun, Z., Zheng, J. et al. 2016. Mixing trees and crops increases land and water use efficiencies in a semi-arid area. Agricultural Water Management 178(C):281–90.CrossRefGoogle Scholar
Bathurst, J. C., Birkinshaw, S. J., Cisneros, F. et al. 2011. Forest impact on floods due to extreme rainfall and snowmelt in four Latin American environments 2: Model analysis. Journal of Hydrology 400:292304.CrossRefGoogle Scholar
Bathurst, J. C. and Iroumé, A. 2014. Quantitative generalizations for catchment sediment yield following forest logging. Water Resources Research 50(11):8383–402. doi:10.1002/2014WR015711.CrossRefGoogle Scholar
Bhatta, L. D., Khadgi, A., Rai, R. K. et al. 2017. Designing community-based payment scheme for ecosystem services: A case from Koshi Hills, Nepal. Environment, Development and Sustainability 20(4):1831–48.Google Scholar
Bosch, J. M. and Hewlett, J. D. 1982. A review of catchment experiments to determine the effect of vegetation changes on water yield and evapotranspiration. Journal of Hydrology 55:323.Google Scholar
Brauman, K. A., Daily, G. C., Duarte, T. K. and Mooney, H. A. 2007. The nature and value of ecosystem services: An overview highlighting hydrologic services. Annual Review of Environment and Resources 32(1):6798.Google Scholar
Brown, A. E., Zhang, L., McMahon, T. A., Western, A. W. and Vertessy, R. A. 2005. A review of paired catchment studies for determining changes in water yield resulting from alterations in vegetation. Journal of Hydrology 310:2861.Google Scholar
Bruijnzeel, L. A. 2001. Hydrology of tropical montane cloud forests: A reassessment. Land Use and Water Resources Research 1:118.Google Scholar
Bruijnzeel, L. A. 2004. Hydrological functions of tropical forests: Not seeing the soil for the trees? Agriculture, Ecosystems and Environment 104(1):185228.Google Scholar
Bruijnzeel, L. A., Mulligan, M. and Scatena, F. N. 2011. Hydrometeorology of tropical montane cloud forests: Emerging patterns. Hydrological Processes 25(3):465–98.Google Scholar
Calder, I. R. 2005. Blue revolution: Integrated land and water resource management, 2nd ed. London: Earthscan.Google Scholar
Chaves, M. M., Pereira, J. S., Maroco, J. et al. 2002. How plants cope with water stress in the field: Photosynthesis and growth. Annals of Botany 89(7):907–16. doi:10.1093/aob/mcf105.Google Scholar
CONAF (Corporación Nacional Forestal) 2016. Estrategia nacional de cambio climático y recursos vegetacionales 2017–2025, Chile. Santiago, Chile: Ministerio de Agricultura, CONAF. Available at: http://portal.mma.gob.cl/wp-content/doc/ENCCRV-2017–2025-web.pdf (Accessed 6 March 2019).Google Scholar
Contreras, S., Santoni, C. S. and Jobbágy, E. G. 2013. Abrupt watercourse formation in a semiarid sedimentary landscape of central Argentina: The roles of forest clearing, rainfall variability and seismic activity. Ecohydrology 6(5):794805.CrossRefGoogle Scholar
Costa, M. H., Botta, A. and Cardille, J. A. 2003. Effects of large-scale changes in land cover on the discharge of the Tocantins River, southeastern Amazonia. Journal of Hydrology 283:206–17.Google Scholar
Creed, I. F. and van Noordwijk, M. (eds.) 2018. Forest and water on a changing planet: Vulnerability, adaptation and governance opportunities. A global assessment report. IUFRO World Series Vol. 38. Vienna: International Union of Forest Research Organizations (IUFRO).Google Scholar
Dalin, C., Konar, M., Hanasaki, N., Rinaldo, A. and Rodriguez-Iturbe, I. 2012. Evolution of the global virtual water trade network. Proceedings of the National Academy of Sciences 109 (16):5989–94.Google Scholar
de Souza, A. L., Fonseca, D. G., Liborio, R. A. and Tanaka, M. O. 2013. Influence of riparian vegetation and forest structure on the water quality of rural low-order streams in SE Brazil. Forest Ecology and Management 298:1218.Google Scholar
Droppelmann, K. J., Lehmann, J., Ephrath, J. E. and Berliner, P. R. 2000. Water use efficiency and uptake patterns in a runoff agroforestry system in an arid environment. Agroforestry Systems 49(3):223–42. doi.org/10.1023/A:1006352623333.Google Scholar
Dye, P. and Versfeld, D. 2007. Managing the hydrological impacts of South African plantation forests: An overview. Forest Ecology and Management 251:121–8.Google Scholar
Ellison, D., Morris, C. E., Locatelli, B. et al. 2017. Trees, forests and water: Cool insights for a hot world. Global Environmental Change 43:5161.Google Scholar
Fahey, B. and Payne, J. 2017. The Glendhu experimental catchment study, upland east Otago, New Zealand: 34 years of hydrological observations on the afforestation of tussock grasslands. Hydrological Processes 31:2921–34. doi:10.1002/hyp.11234.Google Scholar
FAO 2015. Global Forest Resources Assessment 2015. Rome: FAO.Google Scholar
FAO 2018a. SFM Toolbox – Using treated wastewater in forestry and agroforestry in drylands. Available at: www.fao.org/sustainable-forest-management/toolbox/modules/use-of-treated-water-in-forestry-and-agroforestry/basic-knowledge/en/ (Accessed 6 March 2019).Google Scholar
FAO 2018b. Aquastat website. Available at: www.fao.org/nr/aquastat/ (Accessed 6 March 2019).Google Scholar
Farley, K. A., Jobbágy, E. G. and Jackson, R. B. 2005. Effects of afforestation on water yield: A global synthesis with implications for policy. Global Change Biology 11:1565–76.Google Scholar
Filoso, S., Bezerra, M. O., Weiss, K. C. B. and Palmer, M. A. 2017. Impacts of forest restoration on water yield: A systematic review. PLoS ONE 12(8):0183210. doi:org/10.1371/journal.pone.0183210.Google Scholar
Forrester, D. I., Collopy, J. J., Beadle, C. L., Warren, C. R. and Baker, T. G. 2012. Effect of thinning, pruning and nitrogen fertiliser application on transpiration, photosynthesis and water-use efficiency in a young Eucalyptus nitens plantation. Forest Ecology and Management 266:286300.Google Scholar
Global Water Partnership 2017. The need for an integrated approach. Available at: www.gwp.org/en/About/why/the-need-for-an-integrated-approach/ (Accessed 13 February 2019).Google Scholar
Guardian 2019. Jair Bolsonaro launches assault on Amazon rainforest protections. The Guardian, 2 January 2019. Available at: www.theguardian.com/world/2019/jan/02/brazil-jair-bolsonaro-amazon-rainforest-protections (Accessed 13 February 2019).Google Scholar
HLPW 2018. Making every drop count: An agenda for water action. High-Level Panel on Water Outcome Document. Panel convened by United Nations and World Bank Group. Available at: https://sustainabledevelopment.un.org/HLPWater (Accessed 13 February 2019).Google Scholar
Hofer, T. 1993. Himalayan deforestation, changing river discharge, and increasing floods: Myth or reality? Mountain Research and Development 13(3):213–33.CrossRefGoogle Scholar
Hong, S., Piao, S., Chen, A. et al. 2018. Afforestation neutralizes soil pH. Nature Communications 9(520). doi:10.1038/s41467-018–02970-1.CrossRefGoogle ScholarPubMed
Huber, A. and Iroumé, A. 2001. Variability of annual rainfall partitioning for different sites and forest covers in Chile. Journal of Hydrology 248(1–4):7892.Google Scholar
Huber, A., Iroumé, A., Mohr, C. and Frene, C. 2010. Effect of Pinus radiata and Eucalyptus globulus plantations on water resource in the Coastal Range of Biobío region, Chile. Bosque 31(3):219–30.CrossRefGoogle Scholar
Hutton, G. and Varughese, M. 2016. The costs of meeting the 2030 Sustainable Development Goal targets on drinking water, sanitation, and hygiene. Water and Sanitation Program Technical Paper, Washington, DC: World Bank.Google Scholar
Ilstedt, U., Bargués Tobella, A., Bazié, H. R. et al. 2016. Intermediate tree cover can maximize groundwater recharge in the seasonally dry tropics. Scientific Reports 6: 21930.Google Scholar
Iroumé, A., Huber, A. and Schulz, K. 2005. Summer flows in experimental catchments with different forest covers, Chile. Journal of Hydrology 300(1–4):300–13.Google Scholar
Iroumé, A., Mayen, O. and Huber, A. 2006. Runoff and peak flow responses to timber harvest and forest age in southern Chile. Hydrological Processes 20(1):3750.Google Scholar
Iroumé, A. and Palacios, H. 2013. Afforestation and changes in forest composition affect runoff in large river basins with pluvial regime and Mediterranean climate, Chile. Journal of Hydrology 505:113–25. doi:10.1016/j.hydrol.2013.09.031.Google Scholar
Jobbágy, E. G. and Jackson, R. B. 2004. Groundwater use and salinization with grassland afforestation. Global Change Biology 10:1299–312. doi:10.1111/j.1365-2486.2004.00806.x.Google Scholar
Jones, J. A., Achterman, G. L., Augustine, L. A. et al. 2009. Hydrologic effects of a changing forested landscape – challenges for the hydrological sciences. Hydrological Processes 23(18):26992704.Google Scholar
Jones, J., Almeida, A., Cisneros, F. et al. 2017. Forests and water in South America. Hydrological Processes 31(5):972–80. doi:10.1002/hyp.11035.Google Scholar
Khanna, J., Medvigy, D., Fueglistaler, S. and Walko, R. 2017. Regional dry-season climate changes due to three decades of Amazonian deforestation. Nature Climate Change 7(3):200.Google Scholar
Kotru, R., Rathore, B. M. S., Pradhan, N. et al. 2015. Transforming mountain forestry in the Hindu Kush Himalayas: Toward a third-generation forest management paradigm. ICIMOD Working Paper 2015/9. Kathmandu, Nepal: International Centre for Integrated Mountain Development (ICIMOD).Google Scholar
Kotru, R., Sharma, S., Sharma, E. and Hofer, T. 2017. Everybody lives upstream: The watershed approach for the changing climate of Hindu Kush Himalaya. ICIMOD Working Paper 2017/11. Kathmandu, Nepal: ICIMOD.Google Scholar
Kuraś, P. K., Alila, Y. and Weiler, M. 2012. Forest harvesting effects on the magnitude and frequency of peak flows can increase with return period. Water Resources Research 48:W01544. doi:10.1029/2011WR010705.CrossRefGoogle Scholar
Lara, A., Little, C., Urrutia, R. et al. 2009. Assessment of ecosystem services as an opportunity for the conservation and management of native forests in Chile. Forest Ecology and Management 258(4):415–24.Google Scholar
Layton, K. and Ellison, D. 2016. Induced precipitation recycling (IPR): A proposed concept for increasing precipitation through natural vegetation feedback mechanisms. Ecological Engineering 91:553–65.Google Scholar
Little, C., Cuevas, J. G., Lara, A., Pino, M. and Schoenholtz, S. 2015. Buffer effects of streamside native forests on water provision in watersheds dominated by exotic forest plantations. Ecohydrology 8(7):1205–17.Google Scholar
Lorz, C., Abbt-Braun, G., Bakker, F. et al. 2012. Challenges of an integrated water resource management for the Distrito Federal, western central Brazil: Climate, land-use and water resources. Environmental Earth Sciences 65(5):1575–86.Google Scholar
Marc, V. and Robinson, M. 2007. The long-term water balance (1972–2004) of upland forestry and grassland at Plynlimon, mid-Wales. Hydrology and Earth System Science 11(1):4460.CrossRefGoogle Scholar
May, B., Smethurst, P., Carlyle, C. et al. 2009. Review of fertiliser use in Australian forestry. Report prepared for Forest & Wood Products Australia, Melbourne, Australia: Forest & Wood Products Australia. Available at: www.fwpa.com.au/ (Accessed 13 February 2019).Google Scholar
Nelson, E. J., Kareiva, P., Ruckelshaus, M. et al. 2013. Climate change’s impact on key ecosystem services and the human well-being they support in the US. Frontiers in Ecology and the Environment 11(9):483–93.Google Scholar
NRC (National Research Council) 2008. Hydrologic effects of a changing forest landscape. Washington, DC: National Academies Press. Available at: http://nationalacademies.org/wstb (Accessed 13 February 2019).Google Scholar
Oyarzún, C. E. and Huber, A. 2003. Nitrogen export from forested and agricultural watersheds of southern Chile (Exportación de nitrógeno en cuencas boscosas y agrícolas en el sur de Chile). Gayana Botánica 60(1):63–8.Google Scholar
Peck, A. J. and Hatton, T. J. 2003. Salinity and the discharge of salts from catchments in Australia. Journal of Hydrology 272(1–4):191202.Google Scholar
Perakis, S. S. and Hedin, L. O. 2001. Fluxes and fates of nitrogen in soil of an unpolluted old-growth temperate forest, southern Chile. Ecology 82(8):2245–60.Google Scholar
Perakis, S. S. and Hedin, L. O. 2002. Nitrogen loss from unpolluted South American forests mainly via dissolved organic compounds. Nature 415(6870):416.Google Scholar
Perry, T. D. and Jones, J. A. 2017. Summer streamflow deficits from regenerating Douglas-fir forest in the Pacific Northwest, USA. Ecohydrology 10(2):e1790.Google Scholar
Polasky, S., Nelson, E., Pennington, D. and Johnson, K. 2011. The impact of land-use change on ecosystem services, biodiversity and returns to landowners: A case study in the state of Minnesota. Environmental and Resource Economics 48(2):219–42.Google Scholar
Poulos, H. 2018. Why North American cities must thin overgrown forest to improve water supplies. The Source. 5 January [online]. International Water Association. Available at: www.thesourcemagazine.org/trees-became-enemy/ (Accessed 13 February 2019).Google Scholar
Schuller, P., Walling, D. E., Iroumé, A. et al. 2013. Using 137Cs and 210Pbex and other sediment source fingerprints to document suspended sediment sources in small forested catchments in south-central Chile. Journal of Environmental Radioactivity 124:147–59.Google Scholar
Sheil, D. 2018. Forests, atmospheric water and an uncertain future: The new biology of the global water cycle. Forest Ecosystems 5(19). doi:10.1186/s40663-018–0138-y.CrossRefGoogle Scholar
Silveira, L. and Alonso, J. 2009. Runoff modifications due to the conversion of natural grasslands to forests in a large basin in Uruguay. Hydrological Processes 23:320–9. doi:10.1002/hyp.7156.Google Scholar
Singh, V. and Kotru, R. 2018. Sustainable tourism in the Indian Himalayan region. Report of Working Group II. New Delhi: NITI Aayog. Available at: http://niti.gov.in (Accessed 13 February 2019).Google Scholar
Soto-Schönherr, S. and Iroumé, A. 2014. Eficiencia de uso de agua (EUA) de plantaciones forestales y cultivos de secano. Technical report for Bioforest SA (Unpublished).Google Scholar
Soto-Schönherr, S. and Iroumé, A. 2016. How much water do Chilean forests use? A review of interception losses in forest plot studies. Hydrological Processes 30:4674–86. doi:10.1002/hyp.10946.CrossRefGoogle Scholar
Spera, S. A., Galford, G. L., Coe, M. T., Macedo, M. N. and Mustard, J. F. 2016. Land-use change affects water recycling in Brazil’s last agricultural frontier. Global Change Biology 22(10):3405–13.Google Scholar
Su, C. H. and Fu, B. J. 2013. Evolution of ecosystem services in the Chinese Loess Plateau under climatic and land use changes. Global and Planetary Change 101:119–28.Google Scholar
Swann, A. L., Longo, M., Knox, R. G., Lee, E. and Moorcroft, P. R. 2015. Future deforestation in the Amazon and consequences for South American climate. Agricultural and Forest Meteorology 214:1224.Google Scholar
Tew, E. 2016. Jacksonville implements new way to clean wastewater, preserve forest, WNCT, 2 August. Available at: www.wnct.com/news/jacksonville-implements-new-way-to-clean-wastewater-preserve-forest/1091517118 (Accessed 13 February 2019).Google Scholar
Tóth, T., Balog, K., Szabó, A. et al. 2013. Influence of lowland forests on subsurface salt accumulation in shallow groundwater areas. AoB PLANTS 6. doi:10.1093/aobpla/plu054.Google Scholar
UN 2015. The Millennium Development Goals Report. New York: United Nations.Google Scholar
UN 2018. Sustainable Development Goal 6 Synthesis Report 2018 on Water and Sanitation. New York: United Nations.Google Scholar
UNESCO-IHP (International Hydrological Programme) 2014. Water in the post-2015 development agenda and Sustainable Development Goals. Discussion paper prepared for the 21st session of the Intergovernmental Council of the International Hydrological Programme of UNESCO, 18–20 June 2014, UNESCO Headquarters, Paris.Google Scholar
UN Water 2018a. Monitoring Sustainable Development Goal #6. Available at: www.sdg6monitoring.org/ (Accessed 7 July 2018).Google Scholar
UN Water 2018b. About United Nations Water. Available at: www.unwater.org/about-unwater/ (Accessed 7 July 2018).Google Scholar
UN Water 2018c. Water and sanitation interlinkages across the 2030 Agenda for Sustainable Development. Geneva.Google Scholar
van der Ent, R. J., Savenije, H. H. G., Schaefli, B. and Steele-Dunne, S. C. 2010. Origin and fate of atmospheric moisture over continents. Water Resources Research 46(9). doi:10.1029/2010WR009127.Google Scholar
van Dijk, A. and Keenan, R. J. 2007. Planted forests and water in perspective. Forest Ecology and Management 251:19.Google Scholar
Vanham, D., Hoekstra, A., Wada, Y. et al. 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 61314:218–32.Google Scholar
Whitehead, D. and Beadle, C. 2004. Physiological regulation of productivity and water use in Eucalyptus: A review. Forest Ecology and Management 193:113–40.Google Scholar
WWAP (World Water Assessment Programme) 2009. The United Nations World Water Development Report 3: Water in a changing world. Paris: UNESCO and London: Earthscan.Google Scholar
WWF (World Wide Fund for Nature) 2019. Tackling threats that impact the Earth: Deforestation. Available at: www.worldwildlife.org/threats/deforestation (Accessed 13 February 2019).Google Scholar
Yang, H. and Zehnder, A. 2007. ‘Virtual water’: An unfolding concept in integrated water resources management. Water Resources Research 43(12).CrossRefGoogle Scholar
Zhang, M., Liu, N., Harper, R. et al. 2017. A global review on hydrological responses to forest change across multiple spatial scales: Importance of scale, climate, forest type and hydrological regime. Journal of Hydrology 546:4459.Google Scholar
Figure 0

Table 6.1 SDG 6 targets and monitoring indicators for Targets 6.3–6.6

Source: https://sustainabledevelopment.un.org/sdg6
Figure 1

Table 6.2 Potential impacts of SDG 6 indicators on forests

Save book to Kindle

To save this book to your Kindle, first ensure coreplatform@cambridge.org is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

Available formats
×