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DOI | 10.1016/j.quascirev.2020.106389 |
Feedbacks of soil properties on vegetation during the Green Sahara period | |
Chen W.; Ciais P.; Zhu D.; Ducharne A.; Viovy N.; Qiu C.; Huang C. | |
发表日期 | 2020 |
ISSN | 0277-3791 |
卷号 | 240 |
英文摘要 | During the early to middle Holocene, the Sahara received enhanced precipitation and was covered by steppe-like vegetation with a large-scale hydrographic network of lakes, wetlands and fans, which is known as the Green Sahara (GS). However, most coupled land-atmosphere models underestimate the precipitation and vegetation cover, suggesting that critical atmospheric or land surface processes are lacking in those models. Climate-induced vegetation cover change can modify soil texture and physical properties over the long term, which in turn have feedbacks on vegetation. In this study, we examine five plausible soil-vegetation processes in a land surface model, which are expected to increase soil moisture for plants and possibly sustain equilibrium vegetation for a lower rainfall level. The annual precipitation required during the GS epoch to match the modelled vegetation distribution with paleorecords is inferred. Results demonstrate that these soil-vegetation processes have strong positive impacts on vegetation and soil moisture, especially the increase of soil evaporative resistance. After including all soil feedbacks on vegetation, the model requires only a mean precipitation of ∼400 mm/yr to reproduce the pollen-inferred GS vegetation, instead of ∼600 mm/yr when no soil feedback is included. From the mid-Holocene to pre-industrial period, we infer that terrestrial carbon stocks decrease by ∼58 PgC due to the removal of carbon in vegetation, soil and litter pools of the GS. This work highlights the importance of soil-vegetation interactions for simulating dry-region vegetation coverage in models, and the impacts of natural land cover change on carbon budgets in the geological past. © 2020 Elsevier Ltd |
英文关键词 | Bare soil evaporation; Dynamic global vegetation model (DGVM); Mid-holocene; Soil organic carbon; Soil texture; Water infiltration |
语种 | 英语 |
scopus关键词 | Budget control; Carbon; Climate change; Soil moisture; Surface measurement; Textures; Annual precipitation; Evaporative resistances; Hydrographic networks; Land surface modeling; Land-surface process; Mean precipitation; Vegetation coverage; Vegetation distribution; Vegetation; air-soil interaction; carbon sequestration; climate effect; evapotranspiration; feedback mechanism; Holocene; lake ecosystem; soil moisture; soil property; soil-vegetation interaction; steppe; vegetation structure; wetland; Sahara |
来源期刊 | Quaternary Science Reviews
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/151423 |
作者单位 | State Key Laboratory of Biogeology and Environmental Geology, Hubei Key Laboratory of Critical Zone Evolution, School of Earth Sciences, China University of Geosciences, Wuhan, 430074, China; Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette, 91191, France; Sorbonne Université, CNRS, EPHE, Milieux environnementaux, transferts et interaction dans les hydrosystèmes et les sols, Metis, Paris, 75005, France |
推荐引用方式 GB/T 7714 | Chen W.,Ciais P.,Zhu D.,et al. Feedbacks of soil properties on vegetation during the Green Sahara period[J],2020,240. |
APA | Chen W..,Ciais P..,Zhu D..,Ducharne A..,Viovy N..,...&Huang C..(2020).Feedbacks of soil properties on vegetation during the Green Sahara period.Quaternary Science Reviews,240. |
MLA | Chen W.,et al."Feedbacks of soil properties on vegetation during the Green Sahara period".Quaternary Science Reviews 240(2020). |
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