Drought in a warmer, CO <sub>2</sub> -rich climate restricts grassland water use and soil water mixing

Soil water sustains terrestrial life, yet its fate is uncertain under a changing climate. We conducted a deuterium labeling experiment to determine whether elevated atmospheric carbon dioxide (CO<sub>2</sub>), warming, and drought impact soil water storage and transport in a temperate grassland. Elevated CO<sub>2</sub> created a wetter rootzone compared with ambient conditions, whereas warming decreased soil moisture. Soil water remained well mixed in all global change treatments except for summer drought combined with warming and elevated CO<sub>2</sub>. These combined treatments caused the grassland to conserve water and restricted soil water flow to large, rapidly draining pores without mixing with small, slowly draining pores. Our results suggest that drought in a warmer, more CO<sub>2</sub>-rich climate can severely alter grassland ecohydrology by constraining postdrought soil water flow and grassland water use.

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Publication Details

Journal
Science
Published
2025-01-16
DOI
https://doi.org/10.1126/science.ado0734
Citations
16
Primary Topic
Plant Water Relations and Carbon Dynamics
Type
article
Field-Weighted Citation Impact
17.69
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article

Drought in a warmer, CO 2 -rich climate restricts grassland water use and soil water mixing

Ansgar Kahmen, Steffen Birk, Matevž Vremec, Christiane Werner et al.
16 citations
Science
Plant Water Relations and Carbon Dynamics
17.69
article

Drought in a warmer, CO 2 -rich climate restricts grassland water use and soil water mixing

Ansgar Kahmen, Steffen Birk, Matevž Vremec, Christiane Werner, Michael Bahn, Daniel B. Nelson, Maud Tissink, Markus Herndl, Andreas Schaumberger, Nicolas Brüggemann, Angelika Kübert, Jesse Radolinski, Herbert Wachter, Christine Stumpp
article en
16 citations

Abstract

Soil water sustains terrestrial life, yet its fate is uncertain under a changing climate. We conducted a deuterium labeling experiment to determine whether elevated atmospheric carbon dioxide (CO<sub>2</sub>), warming, and drought impact soil water storage and transport in a temperate grassland. Elevated CO<sub>2</sub> created a wetter rootzone compared with ambient conditions, whereas warming decreased soil moisture. Soil water remained well mixed in all global change treatments except for summer drought combined with warming and elevated CO<sub>2</sub>. These combined treatments caused the grassland to conserve water and restricted soil water flow to large, rapidly draining pores without mixing with small, slowly draining pores. Our results suggest that drought in a warmer, more CO<sub>2</sub>-rich climate can severely alter grassland ecohydrology by constraining postdrought soil water flow and grassland water use.

ScienceVol. 387(6731)
University of Graz (AT), University of Freiburg (DE), Forschungszentrum Jülich (DE), University of Basel (CH), Universität Innsbruck (AT), Helsinki Institute of Physics (FI), HBLFA Raumberg-Gumpenstein (AT), University of Maryland, College Park (US), BOKU University (AT)
Openalex Percentile: Top 1%
Plant Water Relations and Carbon Dynamics
17.69
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