Bioenergy with carbon capture and storage (BECCS) is considered an important negative emissions (NEs) technology, but might involve substantial irrigation on biomass plantations. Potential water stress resulting from the additional withdrawals warrants evaluation against the avoided climate change impact. Here we quantitatively assess potential side effects of BECCS with respect to water stress by disentangling the associated drivers (irrigated biomass plantations, climate, land use patterns) using comprehensive global model simulations. By considering a widespread use of irrigated biomass plantations, global warming by the end of the 21st century could be limited to 1.5 °C compared to a climate change scenario with 3 °C. However, our results suggest that both the global area and population living under severe water stress in the BECCS scenario would double compared to today and even exceed the impact of climate change. Such side effects of achieving substantial NEs would come as an extra pressure in an already water-stressed world and could only be avoided if sustainable water management were implemented globally.
The Earth system is facing multiple environmental pressures (e.g. climate change, water shortages, ecosystem degradation), while the need remains to ensure food and water security for a growing world population. Additionally, there is growing interest in NE technologies linked to the desire to achieve the 1.5 °C target without jeopardizing sustainable development goals (SDGs) such as achieving water security. These challenges and their prospective solutions are intrinsically coupled, requiring strong trade-offs to be resolved. One of these dilemmas is centered around freshwater availability and stress. Water stress—affecting about 1.4–4 bn people already depending on the chosen metric1,2,3,4—may strongly increase in the future not only due to population growth, but also due to impacts of global climate change5,6,7,8. For example, a further 8% of world population may be exposed to increasing water stress due to climate change alone9. While mitigation of climate change will thus be imperative to reduce the pressure on freshwater resources (among other benefits)10, the currently pledged emission reductions may not be enough to limit mean global warming to below 2 °C as envisaged in the Paris Agreement11,12, requiring further measures such as active plant-based CO2 sequestration from the atmosphere through dedicated biomass plantations combined with carbon capture and storage (BECCS)13,14,15. BECCS is based on the cultivation of fast-growing plant species, which are assumed to be regularly harvested for their biomass and subsequently processed to bio-fuels (replacing liquid fossil energy carriers), or burned for energy generation (offsetting coal or gas power plants), while the released CO2 is (at least partially) captured16,17. Thus the whole process would remove CO2 from the atmosphere and counteract anthropogenic green-house gas emissions to reduce climate change. The sequestration potential was estimated to be 0.1 GtC yr−1 to 2 GtC yr−1 by 2050 and 0.3 GtC yr−1 to 3.3 GtC yr−1 by 210018,19. Utilization of biomass is supposed to provide substantial amounts of electric energy or liquid fuels (up to 500 EJ yr−1), and is thus assumed to be deployed at large-scale (even without providing negative emissions via CCS) and also rather early in the 21st century (together with afforestation) in contrast to more expensive NE technologies like direct air capture20.
However, at the large-scale required, biomass production is likely to increase the pressure along multiple environmental dimensions locally and globally21,22,23, including increased competition for scarce freshwater resources to the extent that such plantations require irrigation in order to reach anticipated sequestration levels24,25. From a sustainability perspective, it is important to understand how additional water use for bioenergy production affects water stress in relation to the avoided change that would occur in a warming world without irrigated biomass plantations.
We define water stress using an established globally applicable metric: the local ratio of total human water withdrawals to available discharge3,26,27, from which the yearly mean water stress is derived.
To corroborate findings from one earlier regional study that suggested the water stress in a mitigation scenario based on irrigated bioenergy may indeed supersede that of unabated climate change28, we here provide a systematic global-scale analysis comparing water stress in two plausible future scenarios: a world with strong mitigation including (partially irrigated) bioenergy plantations (~600 Mha in 2095) as a contribution to limit mean global warming by the end of the century to around 1.5 °C (hereinafter referred to as scenario BECCS), and one with only marginal extent of bioenergy plantations (~30 Mha in 2095) resulting in warming of 3 °C (CC).
We thus advance earlier studies28,29,30 by globally and spatially explicitly comparing water stress and its drivers between a strong climate change scenario with one where bioenergy is used for mitigation. We take into account available surface water restrictions (e.g. to safeguard environmental flow requirements of river ecosystems) for the irrigation of biomass plantations and cropland. This approach enables us to highlight and quantify trade-offs regarding different levels of water protection, impacts of climate change versus mitigation through BECCS, and also the possible contribution of improved water management to help solve this dilemma. Unlike previous BECCS water demand studies31,32, we apply transient land use projections for both bioenergy and food crops33, which are consistent with future pathways of green-house gas emissions and socio-economic development.
The scenarios are based on data from the Representative Concentration Pathways RCP2.6 (BECCS) and RCP6.0 (CC), both following the "middle of the road" narrative of the Shared Socioeconomic Pathway SSP2, provided by the Inter-Sectoral Impact Model Intercomparison Project (ISIMIP2b)33. Scenarios differ in terms of the degree of climate change, BECCS deployment, and land use change trajectories over the 21st century including differences in the spatial distribution of (rainfed and irrigated) areas with agricultural crops and biomass plantations (Table 1).
To study the beneficial effects of more sustainable water use policies while providing the same amount of biomass as in scenario BECCS, we additionally explore a scenario with irrigated bioenergy plantations that are accompanied by sustainable water management (BECCS+SWM), while all other parameters are chosen for maximum consistency with scenario BECCS. This scenario assumes the preservation of environmental flow requirements (EFRs) and implements advanced on-field water management32,34 on both agricultural and bioenergy sites. EFRs determine a percentage of pristine, undisturbed mean monthly river flow, here following a variable monthly flow (VMF) method35.
Fractions of the local biomass plantation area that are equipped for irrigation (30%—BECCS, 45%—BECCS+SWM) are obtained from a sensitivity analysis, assuming that 50% of the required harvest increase between the Baseline and the ISIMIP2b harvests including technological change is achieved by irrigation (for more details see Methods—determining the bioenergy irrigation amount).
The simulations are performed using the process-based global vegetation and water balance model LPJmL36 forced by climate change scenarios from four General Circulation Models (GCMs) selected in the ISIMIP2b project: HadGEM2-ES, MIROC5, GFDL-ESM2M, IPSL-CM5A-LR. We use an ensemble of GCMs to account for the remaining variation in precipitation projections inherent to GCMs, even when forced with the same RCP37,38.
We compute the water stress index (WSI) for each 0.5 × 0.5 degree grid cell as monthly averages of the present period 2006 to 2015 (Today) and the future period 2090 to 2099, expressed as percentages of human water use (withdrawals for households, industry, and irrigation of biomass plantations and cropland) compared to total discharge. High stress is assumed to prevail in cells where the yearly mean WSI > 40%26,39 (for more details see Methods – Water stress index WSI). From these cells, we calculate sums of global area as well as population under high water stress.
Here, we show that both the global area and the population exposed to high water stress would double in the BECCS scenario compared to today and even exceed the impact of climate change (scenario CC), unless sustainable water management was in place to reduce the pressure on freshwater resources.
Globally aggregated results
We find that by the end of this century (2090–2099), the global population and land area under high water stress will increase sharply in all scenarios without sustainable water management compared to the present (2006–2015). The total land area under high water stress—currently 1023 (982 to 1065) Mha—is simulated to increase in the inter-model mean to 1580 (1520 to 1613) Mha in CC and 1928 (1901 to 1970) Mha in BECCS. The number of people experiencing high water stress—currently 2.28 (2.23–2.32) billion people—increases to 4.15 (4.03–4.24) billion in CC and 4.58 (4.46–4.71) billion in BECCS (Fig. 1, Table S1).
Increases for population under high water stress include the effect of increased world population from 7 billion people in 2010 to 9 billion in 2100 according to SSP240.
Global distribution of water stress
In the following, we focus the presentation of results on simulations under HadGEM2-ES climate projections, which represents an intermediate model response to the applied emission scenario among the group of four GCMs (compare Supplementary Figs. 1 and 2). For results for all other GCMs we refer to the supplementary material (Supplementary Figs. 4, 5 and 6).
The spatial distribution of locations with high water stress in the CC scenario is broadly similar to today’s patterns, but the total area affected as well as the local WSI values increase significantly (Fig. 2), indicating that water stress in current hotspots will persist or even increase. Regional hotspots of WSI increases include the Mediterranean, the Middle East, India, North-East China, and South-East and southern West-Africa (Supplementary Fig. 7). In the BECCS scenario high water stress extends to otherwise unaffected regions (not highly stressed Today nor in CC) e.g. the East of Brazil and large parts of Sub-Saharan Africa (Fig. 2, Supplementary Fig. 8). These are regions where large-scale biomass plantations are assumed (according to the respective ISIMIP2b land use scenario for RCP2.6, see Methods—determining the bioenergy irrigation amount) and in which additional irrigation may therefore be required to increase biomass yields.
Water stress differences between scenarios
All future scenarios exhibit similar or higher water stress almost everywhere compared to Today, with only the Western United States and some locations in Asia showing the opposite behavior (Supplementary Figs. 7 and 8).
Globally, an area of about 2400 Mha (about 16% of the total land surface area) shows a difference larger than ±10% in WSI between the BECCS and CC scenarios. More than two-third (72%) of this area exhibits a higher WSI in the BECCS scenario (Fig. 3a), mostly located in Central and South America, Africa, and Northern Europe. Conversely, on less than one third (28%) of areas (Western US, India, South-East China, and a belt from the Mediterranean region to Kazakhstan), the BECCS scenario demonstrates lower water stress compared to the CC scenario, despite the irrigation for bioenergy.
Thus, without sustainable water management, irrigation of biomass plantations for the purpose of avoiding excessive climate change (3 °C vs. 1.5 °C) would increase water stress significantly in many regions (and also globally, Fig. 1). The effect of higher water stress due to irrigated biomass plantations is consistent among the different GCMs and ranges from 64% in IPSL, over 70% in GFDL, and 72% in HadGEM, to 79% in MIROC (Supplementary Fig. 1). These variations are potentially due to the precipitation and temperature differences between the GCMs (Supplementary Figs. 9 and 10).
Drivers of water stress
Higher WSI in BECCS compared to CC could result from differences in climate, land use, or the irrigation of biomass plantations, as these are the distinctive features in our experimental setup. To determine the attributing cause for the higher WSI in BECCS, we thus ran additional pairs of simulations only varying one of these features while fixing the others (see Methods—attribution of drivers for water stress differences and Fig. 4a–d). Globally, irrigated biomass plantations are the major driver for higher water stress in BECCS (see their extent in Fig. 5) due to the additional freshwater withdrawals. In regions which are simulated to experience a higher WSI in CC, differences are either due to land use or climate (with similar extent). Regarding the difference in land use patterns (Supplementary Fig. 11), we find a large increase in irrigation on areas of the food-producing agriculture (including pastures) in RCP2.6 vs. RCP6.0, which, for example, explains the patterns for the Western United States. The higher water stress in CC compared to BECCS due to climate differences (mostly in Asia) can be attributed to increases in water availability (see precipitation difference in Supplementary Fig. 9).
Comparison of the drivers between GCMs shows relatively high agreement in the Americas and Africa (Fig. 4e). In Europe and Asia, the inter-model variability is higher (no or only two GCMs agree), potentially due to differences in climate inputs and the subsequent impact on river discharge and water availability.
Potentials of sustainable water management
While these results suggest that irrigation for BECCS will lead to stronger increases in water stress than climate change, both globally and regionally, efforts of EFR protection and advanced on-field water management could potentially moderate the effect of irrigated biomass plantations. The respective simulations (scenario BECCS+SWM) indicate a strong reduction of the global area under high water stress to 1224 (1167–1327) Mha. The global population under high water stress is limited to 3.66 (3.47–3.85) billion people. Both area and population in BECCS+SWM are reduced to below the values derived for the CC scenario (Fig. 1). Also the globally aggregated area under increased water stress would be lower (reduction from 72% to 37%; Fig. 3b), indicating that this scenario globally leads to lesser water stress compared to a scenario with stronger climate change and no bioenergy (maps for all GCMs: Supplementary Fig. 2). This demonstrates that irrigation for BECCS, accompanied by policies directed toward more sustainable and effective freshwater use (here, protection of EFRs and improvements in on-farm water use efficiency including on food-producing cropland), could help avoid the aggravation of water stress. However, significant challenges including investment potential and water resource management practices may hamper the implementation of these policies globally. Moreover, there are regions where even these optimal conditions cannot consistently improve water stress conditions (across GCMs) beyond those of CC (Eastern USA, parts of South America, parts of Central and Southern Africa, and parts of Central Europa) (Supplementary Fig. 2). Supplementary Fig. 13 illustrates that, despite SWM, irrigation for BECCS is still the main driver, suggesting that water availability does not allow significant human water withdrawals in these regions.
We conclude that climate mitigation via irrigated BECCS (in an integrated scenario based on RCP2.6), assessed at the global level, will exert similar, or even higher water stress than the mitigated climate change would (in a scenario based on RCP6.0). This confirms (with the exception of the Western United States) results from a previous study for the United States, where irrigated bioenergy plantations were suggested to increase the annual water deficit in comparison to a climate mitigation scenario28, albeit the study has different assumptions on land use and climate trajectories and uses a very different model. Potential hotspots for future water scarcity due to irrigated bioenergy as previously highlighted by the same authors29, do not resemble the patterns which we find, suggesting the need for a larger model intercomparison.
Our results also show that globally, the number of people exposed to severe water stress will generally increase due to climate change and expected population growth3,41. It is thus imperative to minimize additional water demand in an already highly water-stressed world, considering also the strong regional differences highlighted in this study.
We thus explicate the dilemma that on top of technological as well as socio-economic barriers to large-scale BECCS deployment19,42,43, the production of required amounts of biomass (and thus NEs) is further challenged due to freshwater limitations (imposing higher water stress). The reduction of biomass productivity through only cultivating rainfed biomass plantations and discouraging irrigation (50 GtC over the century—Fig. 6); however, might make the difference between 1.5 °C and (likely) 2.0 °C scenarios (87 GtC)44. This highlights the need to include water availability limitation in integrated assessment scenarios that look at stringent mitigation futures such as a 1.5 °C world, because it may change the balance of which NE technologies may appear in those scenarios.
Finally, we show that implementation of more efficient water management (in scenario BECCS+SWM) could offer a synergistic way out of the water stress dilemma. Achieving this requires the stringent implementation of such methods worldwide34,45,46, while the required large economic investments (10–20 billion US$ for Africa alone47) would also help achieving several SDGs48.
Growing evidence suggests that next to the direct influence of irrigation on freshwater availability which we account for here, changes in the evapotranspiration regime due to land use change and especially irrigation may also indirectly influence patterns of local rainfall49,50, and may have remote effects via atmospheric moisture recycling51,52 or effects on specific and relative humidity53. Taking these effects into account requires either a coupled biosphere-atmosphere model or a complex redistribution along atmospheric moisture tracks54 for each climate scenario, which open up avenues for potential future research.
Water stress is just one aspect of the wide-range of potential impacts of climate change. Similarly, also every technology designed to avoid climate change will entail (potentially not yet known) side effects, which can even be beneficial in some regions but detrimental elsewhere. In this regard, more holistic analyses of the consequences of mitigation portfolios are required that take into account all dimensions of the complex Earth system.
The dynamic global vegetation model LPJmL
All simulations are conducted with the process-based Dynamic Global Vegetation Model LPJmL36,55. The global land surface is separated into 67420 cells from a 0.5° × 0.5° global grid. Daily terrestrial carbon fluxes for establishment, growth and productivity of natural vegetation and agriculture on managed land56 are simulated dynamically based on climatic conditions. Hydrological processes consider blue and green water fluxes, connected by a river routing network including dams and reservoirs57,58,59. Sowing dates for 12 crop functional types plus a group of other annual and perennial crops are dynamically calculated60 and calibrated to match national yield statistics61.
Additionally, pastures and two groups of second-generation bioenergy crops (woody and herbaceous) are considered. Woody species resemble temperate willows and poplars or tropical Eucalyptus, while herbaceous species are parameterized as Miscanthus and switchgrass24,62,63. Field data were used to evaluate bioenergy yields against64. A single water use input for SSP2 (to be used in all our scenarios) is prescribed (ISIMIP2b provided multi-model mean domestic and industrial water withdrawal and consumption generated from the ISIMIP2a varsoc runs of WaterGAP, PCR-GLOBWB, and H087). Agricultural areas can be rainfed or irrigated, based on three irrigation techniques: surface, sprinkler, and drip65. To improve water use efficiency, management strategies like mulching, local water storage, and conservation tillage can be applied on a grid-cell level (affecting both cropland and bioenergy plantations)34.
LPJmL can also restrict water withdrawals for irrigation to sustain Environmental Flow Requirement (EFRs), which are calculated from the mean monthly discharges of the last undisturbed period of 1670–1699, before human land use is introduced. Based on the VMF method35, 60% [45%, 30%] of the local discharge in low [intermediate, high] flow months are withhold to secure riverine ecosystems. The flow regime of a given month is defined through comparison with the mean annual flow. Intermediate-flow months are defined by a mean monthly flow of >40% and <80% of the mean annual flow, low flow months below, and high-flow months above this range.
Within a grid-cell crops are assumed to compete with bioenergy plantations for irrigation water. So by cultivating irrigated bioenergy in water-scarce regions or by restricting withdrawals based on EFRs, crop yields are reduced. Possible solutions for potential yield losses resulting from these strict sustainability scenarios have been previously discussed23,66. In our scenarios with water management, the yield decreases are approximately balanced by more effective water management (see Supplementary Fig. 12), which is also applied to cropland67. In our simulations, irrigation water demand, which cannot be met by local surface water availability (or would tap EFRs) can also be fulfilled by available water in neighboring cells. Fossil groundwater resources are not considered, but renewable groundwater resources are included as part of the river discharge (baseflow). Return flows are routed back to the river network.
We acknowledge only using a single simulation model. However, the results reported here are largely controlled by the external climate and land use inputs.
Climate and land use change scenarios
For maximum consistency, LPJmL was only forced with input from the ISIMIP2b protocol33. This includes daily climate data from four General Circulation Models—GCMs—(HadGEM2-ES, MIROC5, GFDL-ESM2M, IPSL-CM5A-LR), as well as cell-based projections of water use7 and GCM-specific land use patterns (including both food and biomass crops) based on the land allocation model MAgPIE68 for RCP2.6 and RCP6.0 based on SSP269. MAgPIE simulations ensure that the food demand required also by the growing population is met, including global trade flows to redistribute products and investment in technological change through which crop productivity can be increased.
LPJmL simulations are performed with an initial spinup of 5000 years of potential natural vegetation (based on preindustrial control-climate) to bring global carbon pools to an equilibrium, followed by 307 years of transient spinup using ISIMIP2b land use patterns from 1700 to 2006. From 2007 to 2100, land use calculated by MAgPIE follows projections aiming at “fulfillment of food, feed and material demand at minimum costs under socio-economic and biophysical constraints”70 (see Supplementary Fig. 12 for the development of total crop harvests). It needs to be noted, that downscaling of land use patterns from MAgPIE regions to the ISIMIP2b grid has not been based on local water availability. For stringent mitigation scenarios, taking into account this potential yield decreasing effect of water limitations on irrigated crop locations might however be desirable.
The climate and land use trajectories used in this study serve as internally consistent scenarios representing a world with limited climate change through large-scale BECCS, which is compared with a strong climate change world. The ISIMIP2b framework is unique for preparing these internally consistent scenarios. Future versions might include more detailed and higher resolution atmospheric as well as land-system processes (e.g. effects of moisture recycling or sea level rise), and potentially even include complex process couplings which could explain global tipping points71. Resilience to complete deforestation, for example, depends on the region and also on the timing of the forest loss72. Including such processes would eventually also allow for even more detailed water stress analyses.
Our results are valid for comparing water stress in the two given climate scenarios with approximate GMT increases (inter-model mean rounded to the closest half-degree) 1.5 °C and 3 °C in 210033 (RCP2.6—1.68 °C and RCP6.0—3.15 °C) and should be understood as such. Any deviation from the given trajectories (faster/slower emission reductions than envisioned, the crossing of tipping points, or newly discovered Earth system behavior) would require the analysis of the corresponding data.
Determining the bioenergy irrigation amount
The ISIMIP2b protocol considers bioenergy plantations for means of energy generation and to realize NEs by BECCS (Fig. 5). Due to land scarcity and potential productivity increases through irrigation, BECCS is likely going to be irrigated to a substantial degree24,32, however in ISIMIP2b irrigation for bioenergy plantations in the land use scenarios is not included. Instead, the land use projections are based on increasing productivity on cropland due to technological change73, which can be invested in, but does not have any effect on the plant physiology (e.g. higher water demand through development of genetically modified cultivars with higher leaf area index). LPJmL does not include such technological change and yield increases require additional irrigation or water management efficiency improvements. Therefore the simulated yields on the given land use patterns are lower than what was initially assumed for ISIMIP2b. We call this scenario Baseline (no irrigation of bioenergy plantations).
Since we focus on quantitative effects of irrigated bioenergy plantations as a productivity increasing management option, we estimated the amount of irrigation, which could reproduce the initially assumed bioenergy harvests to stay consistent with SSP2 and RCP2.6, (under the given water policy and management conditions). We thus performed a sensitivity analysis by equipping a fraction of the bioenergy plantation area share per grid cell from 0% to 60% in 15% steps (irrigation level) and then focused on those scenarios in our analysis, which could explain ~50% of the additional bioenergy productivity increases over the 21st century in the ISIMIP2b demand compared to our baseline scenario with only rainfed bioenergy plants (Fig. 6). The remaining 50% were assumed to be met by technology improvements, which do not have a direct effect on the water cycle (e.g. more efficient usage in labour or capital). The irrigation level that matched this criterion best, is 30% (BECCS). For scenario BECCS+SWM, the irrigation level had to be increased to 45%, due to the withdrawal restrictions for environmental flow protection (for scenario overview see Table S1).
Since the irrigation level was applied globally to all bioenergy grid cells, it also introduced irrigation to cells with low local water availability. Withdrawal restrictions in the BECCS+SWM scenario then effectively turn the cells bioenergy plantations to pure rainfed again.
The employed land use patterns for agriculture and bioenergy as a result of a global optimization would be different if irrigated bioenergy plantations had not been excluded in the ISIMIP2b protocol70. Reaching the same biomass harvest with irrigation potentially requires less plantation area, which could be substituted with other crops. This motivates continued research in defining sustainable regional specific irrigation thresholds and locations based on our water stress maps and a full integration of EFRs and irrigation related parameters into current integrated assessment models.
The ISIMIP2b protocol already includes agricultural residues as additional biomass source for BECCS or bio-fuel production14. Recent studies suggest that there might be an additional potential for utilization of organic wastes, which could reduce the raw biomass demand, and thus reduce land or water requirements74.
Water stress index WSI
The water stress index (WSI) is computed individually for each grid cell on a monthly basis as a 10 year average percentage of human water use (withdrawals) compared to total river discharge (which includes renewable groundwater)26.
From the monthly values, we calculate a mean yearly water stress as the main WSI indicator for this study. In the supplementary information, we perform the same analysis also with cell-based maximum water stress (Supplementary Figs. 3–5, 17), as the water stress of the mostly stressed month (see Supplementary Fig. 18 for a map of these months in scenario BECCS).
Attribution of drivers for water stress differences
The differential water stress maps (Fig. 3) show in which of the two compared scenarios (BECCS or CC) the stress is higher, but they do not explain what the driver for this is. Generally, it could be due to the differences in climate input, land use patterns, or the amount of bioenergy irrigation. To perform the attribution, we analyze six scenarios, where pairs of them only differ in one regard (climate input, land use patterns, or irrigated bioenergy extent). We compare the WSI in these three pairs (CCdiff, LUdiff, and IBdiff). CCdiff is composed of two simulations with climate from RCP6.0 and RCP2.6, but the same RCP2.6 land use without irrigated bioenergy to analyze the climate change contribution. LUdiff is based on two simulations with land use from RCP6.0 and RCP2.6 without irrigated bioenergy, but the same climate from RCP2.6 for the land use contribution. IBdiff is calculated from two simulations with irrigated and non-irrigated bioenergy land use from RCP2.6 and the same climate from RCP2.6 to quantify the irrigated bioenergy component. If a grid cell shows higher water stress in the BECCS scenario, and the absolute of IBdiff is more than 20% higher than that of CCdiff and LUdiff, we mark the cell as Higher WS in scenario BECCS attributable to: irrigated bioenergy (and similar for the other 2 cases). Should 2 or 3 drivers apply at the same time (the differential stresses CCdiff, LUdiff and IBdiff are similar), we mark the cell as undetermined.
Data supporting the main findings of this study are available via https://doi.org/10.5281/zenodo.4297953. Further supplementary data are available from the corresponding author on request.
Model code and analysis scripts are available via https://doi.org/10.5281/zenodo.4297953. Further data are available from the corresponding author on request.
Smakhtin, V., Revenga, C. & Döll, P. A pilot global assessment of environmental water requirements and scarcity. Water Int. 29, 307–317 (2004).
Kummu, M., Ward, P. J., Moel, H. D. & Varis, O. Is physical water scarcity a new phenomenon? global assessment of water shortage over the last two millennia. Environ. Res. Lett. 5, 034006 (2010).
Gosling, S. N. & Arnell, N. W. A global assessment of the impact of climate change on water scarcity. Climatic Change 134, 371–385 (2016).
Mekonnen, M. M. & Hoekstra, A. Y. Four billion people facing severe water scarcity. Sci. Adv. 2, e1500323 (2016).
Hoekstra, A. Y., Mekonnen, M. M., Chapagain, A. K., Mathews, R. E. & Richter, B. D. Global monthly water scarcity: blue water footprints versus blue water availability. PloS ONE 7, e32688 (2012).
Schewe, J. et al. Multimodel assessment of water scarcity under climate change. Proc. Natl Acad Sci. USA 111, 3245–3250 (2014).
Wada, Y. et al. Modeling global water use for the 21st century: Water futures and solutions (wfas) initiative and its approaches. Geoscientific Model Dev. 9, 175–222 (2016).
Heinke, J., Müller, C., Lannerstad, M., Gerten, D. & Lucht, W. Freshwater resources under success and failure of the paris climate agreement. Earth Syst. Dyn. 10, 205–217 (2019).
Gerten, D. et al. Asynchronous exposure to global warming: freshwater resources and terrestrial ecosystems. Environ. Res. Lett. 8, 034032 (2013).
Rockström, J. et al. The world’s biggest gamble. Earth’s Future 4, 465–470 (2016).
Luderer, G. et al. Economic mitigation challenges: how further delay closes the door for achieving climate targets. Environ. Res. Lett. 8, 034033 (2013).
Rogelj, J. et al. Scenarios towards limiting global mean temperature increase below 1.5 °. Nat. Clim. Change 8, 325 (2018).
Minx, J. C. et al. Negative emissions-part 1: research landscape and synthesis. Environ. Res. Lett. 13, 063001 (2018).
Klein, D. et al. The value of bioenergy in low stabilization scenarios: an assessment using REMIND-MAgPIE. Climatic Change 123, 705–718 (2014).
Gasser, T., Guivarch, C., Tachiiri, K., Jones, C. & Ciais, P. Negative emissions physically needed to keep global warming below 2 °C. Nat. Commun. 6, 7958 (2015).
Azar, C., Lindgren, K., Larson, E. & Möllersten, K. Carbon capture and storage from fossil fuels and biomass–costs and potential role in stabilizing the atmosphere. Climatic Change 74, 47–79 (2006).
Caldeira, K., Bala, G. & Cao, L. The science of geoengineering. Annu. Rev. Earth Planet. Sci. 41, 231–256 (2013).
Lenton, T. M. The potential for land-based biological CO2 removal to lower future atmospheric CO2 concentration. Carbon Manag. 1, 145–160 (2010).
Smith, P. et al. Biophysical and economic limits to negative CO2 emissions. Nat. Clim. Change 6, 42 (2016).
Bauer, N. et al. Global energy sector emission reductions and bioenergy use: overview of the bioenergy demand phase of the EMF-33 model comparison. Climatic Change 163, 1553–1568 (2020).
Boysen, L. R., Lucht, W., Gerten, D. & Heck, V. Impacts devalue the potential of large-scale terrestrial CO2 removal through biomass plantations. Environ. Res. Lett. 11, 095010 (2016).
Fuss, S. et al. Negative emissions-part 2: Costs, potentials and side effects. Environ. Res. Lett. 13, 063002 (2018).
Heck, V., Gerten, D., Lucht, W. & Popp, A. Biomass-based negative emissions difficult to reconcile with planetary boundaries. Nat. Clim. Change 8, 151–155 (2018).
Beringer, T., Lucht, W. & Schaphoff, S. Bioenergy production potential of global biomass plantations under environmental and agricultural constraints. GCB Bioenergy 3, 299–312 (2011).
Yamagata, Y. et al. Estimating water-food-ecosystem trade-offs for the global negative emission scenario (IPCC-RCP2.6). Sustainability Sci. 13, 301–313 (2018).
Raskin, P., Gleick, P., Kirshen, P., Pontius, G. & Strzepek, K. Water Futures: Assessment of Long-range Patterns and Problems. Comprehensive Assessment of the Freshwater Resources of the World. (Stockholm Environment Institute, Stockholm, 1997).
Alcamo, J. et al. Global estimates of water withdrawals and availability under current and future “business-as-usual” conditions. Hydrological Sci. J. 48, 339–348 (2003).
Hejazi, M. I. et al. 21st century united states emissions mitigation could increase water stress more than the climate change it is mitigating. Proc. Natl Acad. Sci. 112, 10635–10640 (2015).
Hejazi, M. I. et al. Integrated assessment of global water scarcity over the 21st century under multiple climate change mitigation policies. Hydrol. Earth Syst. Sci. 18, 2859–2883 (2014).
Hu, B., Zhang, Y., Li, Y., Teng, Y. & Yue, W. Can bioenergy carbon capture and storage aggravate global water crisis? Sci. Total Environ. 714, 136856 (2020).
Jans, Y., Berndes, G., Heinke, J., Lucht, W. & Gerten, D. Biomass production in plantations: Land constraints increase dependency on irrigation water. GCB Bioenergy 10, 628–644 (2018).
Stenzel, F., Gerten, D., Werner, C. & Jägermeyr, J. Freshwater requirements of large-scale bioenergy plantations for limiting global warming to 1.5 °C. Environ. Res. Lett. 14, 084001 (2019).
Frieler, K. et al. Assessing the impacts of 1.5 °C global warming-simulation protocol of the inter-sectoral impact model intercomparison project (ISIMIP2b). Geoscientific Model Dev. 10, 4321–4345 (2017).
Jägermeyr, J. et al. Integrated crop water management might sustainably halve the global food gap. Environ. Res. Lett. 11, 025002 (2016).
Pastor, A. V., Ludwig, F., Biemans, H., Hoff, H. & Kabat, P. Accounting for environmental flow requirements in global water assessments. Hydrol. Earth Syst. Sci. 18, 5041–5059 (2014).
Schaphoff, S. et al. LPJmL4 - a dynamic global vegetation model with managed land: Part I—model description. Geosci. Model Dev. Discuss. 2018, 1–59 (2018).
IPCC. The Physical Science Basis. contribution of working group I to the fifth assessment report of the intergovernmental panel on climate change. 2013 (2013).
Woldemeskel, F. M., Sharma, A., Sivakumar, B. & Mehrotra, R. Quantification of precipitation and temperature uncertainties simulated by cmip3 and cmip5 models. J. Geophys. Res.: Atmos. 121, 3–17 (2016).
Vörösmarty, C. J., Green, P., Salisbury, J. & Lammers, R. B. Global water resources: vulnerability from climate change and population growth. Science 289, 284–288 (2000).
K.C., S. & Lutz, W. The human core of the shared socioeconomic pathways: population scenarios by age, sex and level of education for all countries to 2100. Glob. Environ. Change 42, 181 – 192 (2017).
Hanasaki, N. et al. A global water scarcity assessment under shared socio-economic pathways—part 2: Water availability and scarcity. Hydrol. Earth Syst. Sci. 17, 2393–2413 (2013).
Fridahl, M. & Lehtveer, M. Bioenergy with carbon capture and storage (BECCS): Global potential, investment preferences, and deployment barriers. Energy Res. Soc. Sci. 42, 155–165 (2018).
Gough, C. et al. Challenges to the use of BECCS as a keystone technology in pursuit of 1.5 °C. Glob. Sustainability 1, e5 (2018).
Rogelj, J. et al. Energy system transformations for limiting end-of-century warming to below 1. 5 °C. Nat. Clim. Change 5, 519–527 (2015).
Smakhtin, V. Basin closure and environmental flow requirements. Int. J. Water Resour. Dev. 24, 227–233 (2008).
Poff, N. L. & Matthews, J. H. Environmental flows in the anthropocence: past progress and future prospects. Curr. Opin. Environ. Sustainability —Spec. Issue.: Aquat. Mar. Syst. 5, 667–675 (2013).
Rockström, J. & Falkenmark, M. Agriculture: increase water harvesting in Africa. Nature 519, 283–285 (2015).
Jägermeyr, J. Agriculture’s historic twin-challenge toward sustainable water use and food supply for all. Front. Sustain. Food Syst. 4, 35 (2020).
Alter, R. E., Im, E.-S. & Eltahir, E. A. Rainfall consistently enhanced around the Gezira scheme in east Africa due to irrigation. Nat. Geosci. 8, 763–767 (2015).
Szilagyi, J. & Franz, T. E. Anthropogenic hydrometeorological changes at a regional scale: observed irrigation–precipitation feedback (1979–2015) in nebraska, usa. Sustain. Water Resour. Manag. 6, 1 (2020).
Harding, K. J. & Snyder, P. K. Modeling the atmospheric response to irrigation in the great plains. part II: The precipitation of irrigated water and changes in precipitation recycling. J. Hydrometeorol. 13, 1687–1703 (2012).
Pei, L. et al. Effects of irrigation on summer precipitation over the united states. J. Clim. 29, 3541–3558 (2016).
Mishra, V. et al. Moist heat stress extremes in India enhanced by irrigation. Nat. Geosci. 13, 722–728 (2020).
Tuinenburg, O. A. & Staal, A. Tracking the global flows of atmospheric moisture and associated uncertainties. Hydrol. Earth Syst. Sci. 24, 2419–2435 (2020).
Schaphoff, S. et al. LPJmL4—a dynamic global vegetation model with managed land: Part II - model evaluation. Geosci. Model Dev. Discuss. 2018, 1–41 (2018).
Bondeau, A. et al. Modelling the role of agriculture for the 20th century global terrestrial carbon balance. Glob. Change Biol. 13, 679–706 (2007).
Gerten, D., Schaphoff, S., Haberlandt, U., Lucht, W. & Sitch, S. Terrestrial vegetation and water balance-hydrological evaluation of a dynamic global vegetation model. J. Hydrol. 286, 249–270 (2004).
Rost, S. et al. Agricultural green and blue water consumption and its influence on the global water system. Water Resour. Res. 44, W09405 (2008).
Biemans, H. et al. Impact of reservoirs on river discharge and irrigation water supply during the 20th century. Water Resour. Res. 47, W03509 (2011).
Waha, K., van Bussel, L. G. J., Müller, C. & Bondeau, A. Climate-driven simulation of global crop sowing dates. Glob. Ecol. Biogeogr. 21, 247–259 (2012).
Fader, M., Rost, S., Müller, C., Bondeau, A. & Gerten, D. Virtual water content of temperate cereals and maize: present and potential future patterns. J. Hydrol. 384, 218–231 (2010).
Heck, V., Gerten, D., Lucht, W. & Boysen, L. R. Is extensive terrestrial carbon dioxide removal a ‘green’ form of geoengineering? a global modelling study. Glob. Planet. Change 137, 123–130 (2016).
Boysen, L. R. et al. The limits to global-warming mitigation by terrestrial carbon removal. Earth’s Future 5, 463–474 (2017).
Heck, V., Donges, J. F. & Lucht, W. Collateral transgression of planetary boundaries due to climate engineering by terrestrial carbon dioxide removal. Earth Syst. Dyn. 7, 783 (2016).
Jägermeyr, J. et al. Water savings potentials of irrigation systems: global simulation of processes and linkages. Hydrol. Earth Syst. Sci. 19, 3073–3091 (2015).
Gerten, D. et al. Feeding ten billion people is possible within four terrestrial planetary boundaries. Nat. Sustainability 3, 1–9 (2020).
Jägermeyr, J., Pastor, A., Biemans, H. & Gerten, D. Reconciling irrigated food production with environmental flows for sustainable development goals implementation. Nat. Commun. 8, 15900 (2017).
Dietrich, J. P. et al. Magpie 4—a modular open-source framework for modeling global land systems. Geoscientific Model Dev. 12, 1299–1317 (2019).
van Vuuren, D. P. & Carter, T. R. Climate and socio-economic scenarios for climate change research and assessment: reconciling the new with the old. Climatic Change 122, 415–429 (2014).
Bonsch, M. et al. Trade-offs between land and water requirements for large-scale bioenergy production. GCB Bioenergy 8, 11–24 (2016).
Steffen, W. et al. Trajectories of the Earth system in the Anthropocene. Proc. Natl Acad. Sci. 115, 8252–8259 (2018).
Staal, A. et al. Hysteresis of tropical forests in the 21st century. Nat. Commun. 11, 4978 (2020).
Dietrich, J. P., Schmitz, C., Lotze-Campen, H., Popp, A. & Müller, C. Forecasting technological change in agriculture-an endogenous implementation in a global land use model. Technol. Forecast. Soc. Change 81, 236–249 (2014).
Pour, N., Webley, P. A. & Cook, P. J. Potential for using municipal solid waste as a resource for bioenergy with carbon capture and storage (beccs). Int. J. Greenh. Gas. Control 68, 1–15 (2018).
R Core Team. R: A Language and Environment for Statistical Computing. https://www.R-project.org/ (R Foundation for Statistical Computing, 2020).
Original S code by Becker, R. A. & Wilks, A. R., version by Ray Brownrigg. Enhancements by Thomas P Minka and & Alex Deckmyn. Maps: Draw Geographical Maps. R package version 3.3.0. https://CRAN.R-project.org/package=maps (2018).
This study was funded by the CE-Land+ project of the German Research Foundation’s priority program SPP 1689 “Climate Engineering – Risks, Challenges and Opportunities?”. Part of the research was developed in the Young Scientists Summer Program at the International Institute for Applied Systems Analysis, Laxenburg (Austria) with financial support from the German National Member Organization (Association for the Advancement of IIASA). PG and YW are financially supported by EUCP (European Climate Prediction System) project funded by the European Union under Horizon 2020 (Grant Agreement: 776613). We thank Miodrag Stevanović for providing the technological change factors underlying the land use scenarios applied. All figures were created using R75, maps are based on the R package “maps”76.
Open Access funding enabled and organized by Projekt DEAL.
The authors declare that they have no conflict of interest.
Peer review information Nature Communications thanks Mathias Fridahl, Mesfin Mekonnen and the other, anonymous, reviewer(s) for their contribution to the peer review of this work. Peer reviewer reports are available.
Publisher’s note Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
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Stenzel, F., Greve, P., Lucht, W. et al. Irrigation of biomass plantations may globally increase water stress more than climate change. Nat Commun 12, 1512 (2021). https://doi.org/10.1038/s41467-021-21640-3
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