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Water scarcity and fish imperilment driven by beef production

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Human consumption of freshwater is now approaching or surpassing the rate at which water sources are being naturally replenished in many regions, creating water shortage risks for people and ecosystems. Here we assess the impact of human water uses and their connection to water scarcity and ecological damage across the United States, identify primary causes of river dewatering and explore ways to ameliorate them. We find irrigation of cattle-feed crops to be the greatest consumer of river water in the western United States, implicating beef and dairy consumption as the leading driver of water shortages and fish imperilment in the region. We assess opportunities for alleviating water scarcity by reducing cattle-feed production, finding that temporary, rotational fallowing of irrigated feed crops can markedly reduce water shortage risks and improve ecological sustainability. Long-term water security and river ecosystem health will ultimately require Americans to consume less beef that depends on irrigated feed crops.
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https://doi.org/10.1038/s41893-020-0483-z
1Sustainable Waters, Crozet, VA, USA. 2University of Virginia, Charlottesville, VA, USA. 3Water Asset Management, San Francisco, CA, USA. 4USDA
Forest Service, Southern Research Station, Otto, NC, USA. 5Department of Geography and Spatial Sciences, University of Delaware, Newark, DE, USA.
6Department of Plant and Soil Sciences, University of Delaware, Newark, DE, USA. 7Data Science Institute, Columbia University, New York, NY, USA.
8Darden School of Business, University of Virginia, Charlottesville, VA, USA. 9Twente Water Center, University of Twente, Enschede, The Netherlands.
10Institute of Water Policy, Lee Kuan Yew School of Public Policy, National University of Singapore, Singapore, Singapore. 11Institute of Urban Development,
Nanjing Audit University, Nanjing, Jiangsu, China. 12Civil Engineering Department, Kansas State University, Manhattan, KS, USA. 13Department of
Environmental Science, Baylor University, Waco, TX, USA. 14Robert B. Daugherty Water for Food Global Institute, University of Nebraska, Lincoln, NE, USA.
15Northern Arizona University, Flagstaff, AZ, USA. 16Lehigh University, Bethlehem, PA, USA. 17University of Victoria, Victoria, British Columbia, Canada.
e-mail: brian@sustainablewaters.org
Water shortages have afflicted human societies for thou-
sands of years1. As population centres grow and farmlands
expand, freshwater consumption typically increases until
renewable water supplies are fully utilized (for example, in Fig. 1);
at this point, water users and freshwater ecosystems become highly
vulnerable to water shortages during drier periods2. Historically,
water shortages had local causes and consequences, involving only
the communities that were directly dependent on an overused river
or aquifer. Today, however, with trade networks encircling the globe,
demand for asparagus in the United Kingdom can contribute to the
depletion of an aquifer in the Peruvian desert3,4 and water shortages
in the Central Valley of California can affect the availability and price
of almonds and pistachios imported into the European Union5.
Climate change exacerbates water shortages by affecting both
water supplies and water demands. Higher temperatures increase
evapotranspiration, reducing aquifer recharge and watershed run-
off6. For example, Udall and Overpeck attributed one-third of recent
declines in Colorado River flows (19% below average during 2000–
2014) to temperature increases7. The Intergovernmental Panel on
Climate Change expressed high confidence that irrigation—the
largest water-using sector globally—will increase in coming decades
due to increased evapotranspiration6.
Human-induced depletion of river flows has deleteriously
affected freshwater species and ecosystems across the globe8,9 and
is a leading cause of fish imperilment in the US1012. Richter etal.12
documented that 62% of sub-watersheds in the western US contain
at least one species endangered by flow depletion, with a total of 367
plant and animal species affected, including two-thirds of all native
fish species in the Colorado River basin. To protect species listed
under the US Endangered Species Act, water regulators have been
forced to curtail water use for irrigation in some watersheds, lead-
ing to severe political controversy and economic hardship13,14. The
annual cost of recovering Endangered Species Act-listed fish species
(more than US$800 million per year) now exceeds expenditures for
all other animal and plant groups combined15.
Water shortages have increased in both frequency and geographic
extent in the US and globally16,17. However, some recent water short-
ages have begun to stimulate policy responses. A severe drought in
California during 2012–2016 led to record levels of river and aquifer
depletion across the state and US$2.7 billion in agricultural losses in
2015 alone, provoking mandatory state-wide water use reductions
and legislation requiring preparation of sustainable groundwater-
management plans18,19. In recent decades, water extractions from
the Colorado River have exceeded total river flow, causing rapid
depletion of water-storage reservoirs (Fig. 1). In response, state and
federal water agencies are preparing demand-management plans to
stabilize reservoir levels and avoid mandatory reductions in water
deliveries to states sharing the basin’s water2022.
For water-management plans and policies to succeed, they need
sufficiently detailed and accurate information that can enrich under-
standing of the causes of water shortages and help guide decision
making around potential solutions. Here we assess river flow deple-
tion across the US, identify direct and indirect drivers of this deple-
tion, and assess options to reduce vulnerability to water shortages.
Our findings led to closer examination of the water use and eco-
logical impacts associated with irrigation of cattle-feed crops. We
Water scarcity and fish imperilment driven by
beef production
Brian D. Richter 1,2 ✉ , Dominique Bartak3, Peter Caldwell4, Kyle Frankel Davis 5,6,7,
Peter Debaere8, Arjen Y. Hoekstra 9,10, Tianshu Li 11, Landon Marston 12, Ryan McManamay 13,
Mesfin M. Mekonnen 14, Benjamin L. Ruddell15, Richard R. Rushforth15 and Tara J. Troy 16,17
Human consumption of freshwater is now approaching or surpassing the rate at which water sources are being naturally replen-
ished in many regions, creating water shortage risks for people and ecosystems. Here we assess the impact of human water
uses and their connection to water scarcity and ecological damage across the United States, identify primary causes of river
dewatering and explore ways to ameliorate them. We find irrigation of cattle-feed crops to be the greatest consumer of river
water in the western United States, implicating beef and dairy consumption as the leading driver of water shortages and fish
imperilment in the region. We assess opportunities for alleviating water scarcity by reducing cattle-feed production, finding
that temporary, rotational fallowing of irrigated feed crops can markedly reduce water shortage risks and improve ecological
sustainability. Long-term water security and river ecosystem health will ultimately require Americans to consume less beef that
depends on irrigated feed crops.
NATURE SUSTAINABILITY | VOL 3 | APRIL 2020 | 319–328 | www.nature.com/natsustain 319
Content courtesy of Springer Nature, terms of use apply. Rights reserved
... We built on the work of Richter et al. 3 by extending the hydrological simulation period from 1981 to 2019 and integrating new detailed monthly estimates of irrigation use for 30 individual crops (accounting for 94% of the total irrigated area and 95% of irrigation water consumption in the United States, Supplementary Table 1). We estimated monthly hydrological balances using the water supply stress index (WaSSI) ecosystem services model, which can simulate the hydrological impact of extractions from surface water and groundwater sources separately as well as hydrological interactions between river flow and groundwater 31,32 . ...
... We estimated monthly hydrological balances using the water supply stress index (WaSSI) ecosystem services model, which can simulate the hydrological impact of extractions from surface water and groundwater sources separately as well as hydrological interactions between river flow and groundwater 31,32 . Richter et al. 3 used static irrigation requirements based on annual average crop water requirements from 1996 to 2005. We have improved upon this approach by estimating crop water requirements at a monthly time step for each month from 1981 to 2019, which allowed us to capture the seasonal and interannual variability of crop water use, facilitating our assessment of trends and changing crop mixes over time. ...
... There are 2,099 HUC8 sub-basins in the conterminous United States, each with a mean area of 3,750 km 2 . All WaSSI input data and assumptions used in this study are exactly as described by Richter et al. 3 , but we included updated climate and land use data for an extended period of 1981-2019, as described below, and used substantially improved estimates of crop water consumption, also described below. An important feature of our hydrological model is the tracking of surface water flows from upstream to downstream sub-basins within each drainage network. ...
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... Across the United States, cities with high SCD values were less likely to experience food shocks of increasing intensity than cities with low SCD values ( Supplementary Fig. 2). While the exposure of cities' food supply chains to water stress did not vary considerably between food sectors, it did reveal a marked spatial pattern, characterized by cities in the west being more exposed to water stress than those in the east through food ows 30,31 (Supplementary Fig. 3). On average, across food sectors, the SCE of western cities was 0.50 versus 0.19 in eastern cities (p < 0.001). ...
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در چند دهه اخیر، سرانه تولید ناخالص داخلی (GDP) چین، هند و سایر اقتصادهای نوظهور به‌طور قابل توجهی افزایش یافته است. بر اساس گزارش بانک جهانی، سرانه تولید ناخالص داخلی چین و هند در سال 2017 به ترتیب ده و سه برابر بیشتر از 30 سال پیش است. در این زمینه، مجال کمی برای دیدگاه «محدودیت‌های رشد» وجود دارد که یادآور دهه 1970 و باشگاه رم در مورد بقیه جهان است . از آنجا که رشد اقتصادی این پتانسیل را دارد که تفاوت‌های درآمدی را در سطح بین‌المللی به حداقل برساند، اقتصادهای پیشرفته در موقعیتی نیستند که «محدودیت‌هایی برای رشد» بر بقیه جهان اعمال کنند. ازاین‌رو، یک راهکار احتمالی، رشد «خنثی از منابع»؛ یا در زمینه مورد مطالعه ما، رشد «خنثی از آب» است. به‌طور کلی، مصرف آب نمی‌تواند به افزایش ادامه دهد. باید محدودیتی برای مصرف کلی آب وجود داشته باشد و جوامع باید با آب کمتر کارهای بیشتری انجام دهند (کارایی بالاتری داشته باشند)، که بنا به ضرورت، افزایش بهره‌وری آب را به همراه دارد. درحالی‌که بهبود پایدار بهره‌وری آب ممکن است یک هدف عالی به نظر برسد، مهم است که تأکید شود که این یک موضوع کاملاً در دسترس می‌باشد.
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Between 2000 and 2014, annual Colorado River flows averaged 19% below the 1906-1999 average, the worst 15-year drought on record. At least one-sixth to one-half (average at one-third) of this loss is due to unprecedented temperatures (0.9°C above the 1906-99 average), confirming model-based analysis that continued warming will likely further reduce flows. Whereas it is virtually certain that warming will continue with additional emissions of greenhouse gases to the atmosphere, there has been no observed trend towards greater precipitation in the Colorado Basin, nor are climate models in agreement that there should be a trend. Moreover, there is a significant risk of decadal and multidecadal drought in the coming century, indicating that any increase in mean precipitation will likely be offset during periods of prolonged drought. Recently published estimates of Colorado River flow sensitivity to temperature combined with a large number of recent climate model-based temperature projections indicate that continued business-as-usual warming will drive temperature-induced declines in river flow, conservatively -20% by mid-century and -35% by end–century, with support for losses exceeding -30% at mid-century and -55% at end-century. Precipitation increases may moderate these declines somewhat, but to date no such increases are evident and there is no model agreement on future precipitation changes. These results, combined with the increasing likelihood of prolonged drought in the river basin, suggest that future climate change impacts on the Colorado River flows will be much more serious than currently assumed, especially if substantial reductions in greenhouse gas emissions do not occur. This article is protected by copyright. All rights reserved.