Responses of vegetation greenness and carbon cycle to extreme droughts in China

被引:117
作者
Deng, Ying [1 ]
Wang, Xuhui [1 ]
Wang, Kai [1 ]
Ciais, Philippe [2 ]
Tang, Shuchang [1 ]
Jin, Lei [1 ]
Li, Lili [1 ]
Piao, Shilong [1 ,3 ,4 ]
机构
[1] Peking Univ, Coll Urban & Environm Sci, Sino French Inst Earth Syst Sci, Beijing 100871, Peoples R China
[2] CEA CNRS UVSQ, Lab Sci Climat & Environm, F-91191 Gif Sur Yvette, France
[3] Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Alpine Ecol & Biodivers, Beijing 100085, Peoples R China
[4] Chinese Acad Sci, Ctr Excellence Tibetan Earth Sci, Beijing 100085, Peoples R China
基金
中国国家自然科学基金;
关键词
Drought; Extreme climate; Vegetation greenness; Carbon cycle; GROSS PRIMARY PRODUCTIVITY; NET PRIMARY PRODUCTION; CLIMATE EXTREMES; TERRESTRIAL GROSS; IMPACTS; FLUXES; GROWTH; HEAT; ECOSYSTEMS; BALANCE;
D O I
10.1016/j.agrformet.2020.108307
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Increasing drought stress under climate change exerting large impacts on vegetation has aroused growing concern, yet how vegetation greenness and carbon cycle respond to extreme drought is not well understood. In this paper, we studied this issue with various data sources including satellite observation, flux sites upscaling estimation, atmospheric inversion, and Dynamic Global Vegetation Model (DGVM) simulations over China during the period 2000-2015. We found a highly consistent negative response of greenness and carbon fluxes to extreme droughts, with the largest reduction in Gross Primary Productivity (GPP, a standardized anomaly of -1.26 similar to -0.33), a slightly smaller extent decrease of Net Ecosystem Productivity (NEP, -0.74 similar to -0.14) due to concurrent decrease of respiration, and reduced Leaf Area Index (LAI, -0.39 similar to -0.20). Besides, there was a large spatial heterogeneity across different regions and biomes, where Loess Plateau was one of the most vulnerable regions. The ambient climate conditions were found to modulate the drought response. Drought sensitivity of greenness and GPP peaked where mean annual temperature is around 25 degrees C, while that of NEP decreased along increasing precipitation gradients.
引用
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页数:9
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