Plant phenology changes and drivers on the Qinghai-Tibetan Plateau (Jul, 10.1038/s43017-022-00317-5, 2022)

被引:37
作者
Shen, Miaogen
Wang, Shiping
Jiang, Nan
Sun, Jianping
Cao, Ruyin
Ling, Xiaofang
Fang, Bo
Zhang, Lei
Zhang, Lihao
Xu, Xiyan
Lv, Wangwang
Li, Baolin
Sun, Qingling
Meng, Fandong
Jiang, Yuhao
Dorji, Tsechoe
Fu, Yongshuo
Iler, Amy
Vitasse, Yann
Steltzer, Heidi
Ji, Zhenming
Zhao, Wenwu
Piao, Shilong
Fu, Bojie
机构
[1] State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing
[2] State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing
[3] School of Resources and Environment, University of Electronic Science and Technology of China, Chengdu
[4] Key Laboratory of Regional Climate-Environment for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing
[5] State Key Laboratory of Resources and Environmental Information System, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing
[6] School of Atmospheric Sciences, Sun Yat-sen University, Zhuhai
[7] Department of Ecology, College of Urban and Environmental Sciences, and Key Laboratory for Earth Surface Processes of the Ministry of Education, Peking University, Beijing
[8] Academy of Forest Inventory and Planning, National Forestry and Grassland Administration, Beijing
[9] College of Water Sciences, Beijing Normal University, Beijing
[10] Rocky Mountain Biological Laboratory, Crested Butte, CO
[11] Forest Dynamics Unit, Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Birmensdorf
[12] Environment & Sustainability Department, Fort Lewis College, Durango, CO
基金
中国国家自然科学基金;
关键词
D O I
10.1038/s43017-022-00340-6
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The ongoing phenological changes in vegetation on the Qinghai–Tibetan Plateau could modify land surface and atmospheric processes. In this Review, we summarize these changes, their drivers and the resulting impacts. The start of the growing season advanced by 9.4 ± 2.2 days during 1982–1999 and 8.3 ± 2.0 days over 2000–2020, and the end of season delayed by 8.2 ± 1.9 days during 2000–2020. The main identified drivers of these changes are warming temperatures and increasing precipitation, but their impacts vary substantially across the Qinghai–Tibetan Plateau. Other factors, such as grazing and nitrogen deposition, also potentially influence phenological changes, but these relationships are poorly constrained. In manipulation experiments, grazing and nitrogen addition have no individual effects on most phenophase timings at the population level, but nitrogen addition markedly delays flowering. Additionally, there are carry-over effects between phenophases that control subsequent temperature and precipitation responses. Phenological changes in turn could alter species interactions, modulate carbon and water cycling, and affect Asian monsoons and spring rainfall over eastern China, but evidence of these interactions is limited. Harmonization of remote-sensing-based and in situ observations, and simultaneous testing of both biotic and abiotic factors, are needed for a mechanistic understanding of Qinghai–Tibetan Plateau phenology dynamics. © 2022, Springer Nature Limited.
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页码:717 / 717
页数:1
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[1]  
Shen MG, 2022, NAT REV EARTH ENV, V3, P633, DOI 10.1038/s43017-022-00317-5