EGU21-9028
https://doi.org/10.5194/egusphere-egu21-9028
EGU General Assembly 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Soil moisture-atmosphere feedbacks mitigate declining water availability in drylands

Sha Zhou1, A. Park Williams2, Benjamin Lintner3, Alexis Berg4, Yao Zhang5, Trevor Keenan5, Benjamin Cook6, Stefan Hagemann7, Sonia Seneviratne8, and Pierre Gentine1
Sha Zhou et al.
  • 1Department of Earth and Environmental Engineering, Columbia University, New York, NY, USA (sz2766@columbia.edu)
  • 2Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA
  • 3Department of Environmental Sciences, Rutgers, The State University of New Jersey, New Brunswick, NJ, USA
  • 4Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA, USA
  • 5Department of Environmental Science, Policy and Management, UC Berkeley, CA, USA
  • 6NASA Goddard Institute for Space Studies, New York, NY, USA
  • 7Helmholtz-Zentrum Geesthacht, Institute of Coastal Research, Geesthacht, Germany
  • 8Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland

Global warming alters surface water availability (precipitation minus evapotranspiration, P-E) and hence freshwater resources. However, the influence of land-atmosphere feedbacks on future P-E changes and the underlying mechanisms remain unclear. Here we demonstrate that soil moisture (SM) strongly impacts future P-E changes, especially in drylands, by regulating evapotranspiration and atmospheric moisture inflow. Using modeling and empirical approaches, we find a consistent negative SM feedback on P-E, which may offset ~60% of the decline in dryland P-E otherwise expected in the absence of SM feedbacks. The negative feedback is not caused by atmospheric thermodynamic responses to declining SM, but rather reduced SM, in addition to limiting evapotranspiration, regulates atmospheric circulation and vertical ascent to enhance moisture transport into drylands. This SM effect is a large source of uncertainty in projected dryland P-E changes, underscoring the need to better constrain future SM changes and improve representation of SM-atmosphere processes in models.

How to cite: Zhou, S., Williams, A. P., Lintner, B., Berg, A., Zhang, Y., Keenan, T., Cook, B., Hagemann, S., Seneviratne, S., and Gentine, P.: Soil moisture-atmosphere feedbacks mitigate declining water availability in drylands, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-9028, https://doi.org/10.5194/egusphere-egu21-9028, 2021.

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