65% cover is the sustainable vegetation threshold on the Loess Plateau

被引:6
|
作者
Chen, Yi-ping [1 ]
Wang, Kai-bo [1 ]
Fu, Bo-jie [2 ]
Wang, Yan-fen [3 ]
Tian, Han-wen [1 ,3 ]
Wang, Yi [1 ]
Zhang, Yi [1 ]
机构
[1] Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess Sci, Xian 700061, Peoples R China
[2] Chinese Acad Sci, Res Ctr Ecoenvironm Sci, Beijing 100085, Peoples R China
[3] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
基金
中国国家自然科学基金;
关键词
Climate change; Loss plateau; Vegetation change; Sustainable development; Yellow River; CARBON SEQUESTRATION; CHINA; CLIMATE; TEMPERATURE; IMPACTS; ALASKA; GREEN; GRAIN;
D O I
10.1016/j.ese.2024.100442
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Global temperatures will continue to increase in the future. The -640,000-km2 Loess Plateau (LP) is a typical arid and semi-arid region in China. Similar regions cover -41% of the Earth, and its soils are some of the most severely eroded anywhere in the world. It is very important to understand the vegetation change and its ecological threshold under climate change on the LP for the sustainable development in the Yellow River Basin. However, little is known about how vegetation on the LP will respond to climate change and what is the sustainable threshold level of vegetation cover on the LP. Here we show that the temperature on the LP has risen 0.27 degrees C per decade over the past 50 years, a rate that is 30% higher than the average warming rate across China. During historical times, vegetation change was regulated by environmental factors and anthropogenic activities. Vegetation coverage was about 53% on the LP from the Xia Dynasty to the Spring and Autumn and Warring States period. Over the past 70 years, however, the environment has gradually improved and the vegetation cover had increased to -65% by 2021. We forecast future changes of vegetation cover on the LP in 2030s, in 2050s and in 2070s using SDM (Species Distribution Model) under Low-emission scenarios, Medium-emission scenarios and High-emission scenarios. An average value of vegetation cover under the three emission scenarios will be 64.67%, 62.70% and 61.47%, respectively. According to the historical record and SDM forecasts, the threshold level of vegetation cover on the LP is estimated to be 53e65%. Currently, vegetation cover on the LP has increased to the upper limit of the threshold value (-65%). We conclude that the risk of ecosystem collapse on the LP will increase with further temperature increases once the vegetated area and density exceed the threshold value. It is urgent to adopt sustainable strategies such as stopping expanding vegetation area and scientifically optimizing the vegetation structure on the LP to improve the ecological sustainability of the Yellow River Basin. (c) 2024 The Authors. Published by Elsevier B.V. on behalf of Chinese Society for Environmental Sciences, Harbin Institute of Technology, Chinese Research Academy of Environmental Sciences. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).
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页数:9
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