Soil moisture-atmosphere feedbacks mitigate declining water availability in drylands

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...

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Veröffentlicht in:	Nature climate change 2021-01, Vol.11 (1), p.38-44
Hauptverfasser:	Zhou, Sha, Williams, A. Park, Lintner, Benjamin R., Berg, Alexis M., Zhang, Yao, Keenan, Trevor F., Cook, Benjamin I., Seneviratne, Sonia I., Gentine, Pierre
Format:	Artikel
Sprache:	eng
Schlagworte:	704/106 704/242 706/2805 Arid lands Arid zones Ascent Atmosphere Atmospheric circulation Atmospheric models Atmospheric moisture Availability Climate Change Climate Change/Climate Change Impacts Climate models Earth and Environmental Science Environment Environmental Law/Policy/Ecojustice Evapotranspiration Feedback Freshwater Freshwater resources Global warming Inflow Inland water environment Meteorology And Climatology Negative feedback Soil Soil moisture Surface water Surface water availability Water availability
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