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Notable shifts beyond pre-industrial streamflow and soil moisture conditions transgress the planetary boundary for freshwater change

Porkka, Miina; Virkki, Vili; Wang-Erlandsson, Lan; Gerten, Dieter; Gleeson, Tom; Mohan, Chinchu; Fetzer, Ingo; Jaramillo, Fernando; Staal, Arie; te Wierik, Sofie; Tobian, Arne; van der Ent, Ruud; Döll, Petra; Flörke, Martina; Gosling, Simon N.; Hanasaki, Naota; Satoh, Yusuke; Müller Schmied, Hannes; Wanders, Niko; Famiglietti, James S.; Rockström, Johan; Kummu, Matti

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Authors

Miina Porkka

Vili Virkki

Lan Wang-Erlandsson

Dieter Gerten

Tom Gleeson

Chinchu Mohan

Ingo Fetzer

Fernando Jaramillo

Arie Staal

Sofie te Wierik

Arne Tobian

Ruud van der Ent

Petra Döll

Martina Flörke

Dr SIMON GOSLING SIMON.GOSLING@NOTTINGHAM.AC.UK
Professor of Climate Risks and Environmental Modelling

Naota Hanasaki

Yusuke Satoh

Hannes Müller Schmied

Niko Wanders

James S. Famiglietti

Johan Rockström

Matti Kummu



Abstract

Human actions compromise the many life-supporting functions provided by the freshwater cycle. Yet, scientific understanding of anthropogenic freshwater change and its long-term evolution is limited. Here, using a multi-model ensemble of global hydrological models, we estimate how, over a 145-year industrial period (1861–2005), streamflow and soil moisture have deviated from pre-industrial baseline conditions (defined by 5th–95th percentiles, at 0.5° grid level and monthly timestep over 1661–1860). Comparing the two periods, we find an increased frequency of local deviations on ~45% of land area, mainly in regions under heavy direct or indirect human pressures. To estimate humanity’s aggregate impact on these two important elements of the freshwater cycle, we present the evolution of deviation occurrence at regional to global scales. Annually, local streamflow and soil moisture deviations now occur on 18.2% and 15.8% of global land area, respectively, which is 8.0 and 4.7 percentage points beyond the ~3 percentage point wide pre-industrial variability envelope. Our results signify a substantial shift from pre-industrial streamflow and soil moisture reference conditions to persistently increasing change. This indicates a transgression of the new planetary boundary for freshwater change, which is defined and quantified using our approach, calling for urgent actions to reduce human disturbance of the freshwater cycle.

Journal Article Type Article
Acceptance Date Jan 9, 2024
Online Publication Date Mar 4, 2024
Publication Date Mar 4, 2024
Deposit Date Jan 29, 2024
Publicly Available Date Mar 5, 2024
Journal Nature Water
Electronic ISSN 2731-6084
Publisher Nature Research
Peer Reviewed Peer Reviewed
DOI https://doi.org/10.1038/s44221-024-00208-7
Keywords Environmental sciences Hydrology; Sustainability
Public URL https://nottingham-repository.worktribe.com/output/30510679
Publisher URL https://www.nature.com/articles/s44221-024-00208-7
Additional Information Received: 24 May 2023; Accepted: 30 January 2024; First Online: 4 March 2024; : The authors declare no competing interests.

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