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Abstract
Drylands cover 41% of Earth’s surface and are the largest source of interannual variability in the global carbon sink. Drylands are projected to experience accelerated expansion over the next century, but the implications of this expansion on variability in gross primary production (GPP) remain elusive. Here we show that by 2100 total dryland GPP will increase by 12 ± 3% relative to the 2000–2014 baseline. Because drylands will largely expand into formerly productive ecosystems, this increase in dryland GPP may not increase global GPP. Further, GPP per unit dryland area will decrease as degradation of historical drylands outpaces the higher GPP of expanded drylands. Dryland expansion and climate-induced conversions among sub-humid, semi-arid, arid, and hyper-arid subtypes will lead to substantial changes in regional and subtype contributions to global dryland GPP variability. Our results highlight the vulnerability of dryland subtypes to more frequent and severe climate extremes and suggest that regional variations will require different mitigation strategies.
Earth’s drylands are expected to expand due to climate change, but how this will affect vegetation remains unclear. Here the authors use models to show that despite expansion, primary productivity in drylands is likely to increase through the 21st Century.
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1 Washington State University, Department of Civil and Environmental Engineering, WA, USA (GRID:grid.30064.31) (ISNI:0000 0001 2157 6568); Lanzhou University, Key Laboratory for Semi-Arid Climate Change of the Ministry of Education, College of Atmospheric Sciences, Lanzhou, China (GRID:grid.32566.34) (ISNI:0000 0000 8571 0482)
2 Washington State University, Department of Civil and Environmental Engineering, WA, USA (GRID:grid.30064.31) (ISNI:0000 0001 2157 6568)
3 Lanzhou University, Key Laboratory for Semi-Arid Climate Change of the Ministry of Education, College of Atmospheric Sciences, Lanzhou, China (GRID:grid.32566.34) (ISNI:0000 0000 8571 0482); CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing, China (GRID:grid.9227.e) (ISNI:0000000119573309)
4 Fudan University, Department of Atmospheric and Oceanic Sciences & Institute of Atmospheric Sciences, Shanghai, China (GRID:grid.8547.e) (ISNI:0000 0001 0125 2443); Lanzhou University, Key Laboratory for Semi-Arid Climate Change of the Ministry of Education, College of Atmospheric Sciences, Lanzhou, China (GRID:grid.32566.34) (ISNI:0000 0000 8571 0482)
5 Boston University, Department of Earth and Environment, Boston, USA (GRID:grid.189504.1) (ISNI:0000 0004 1936 7558)
6 Chinese Academy of Sciences, Northwest Institute of Eco-Environment and Resources, Lanzhou, China (GRID:grid.9227.e) (ISNI:0000000119573309)
7 Pacific Northwest National Laboratory, Atmospheric Sciences and Global Change Division, Richland, USA (GRID:grid.451303.0) (ISNI:0000 0001 2218 3491)