Revegetation affects the response of land surface phenology to climate in Loess Plateau, China

被引:7
|
作者
Wang, Lvlv [1 ,2 ]
She, Dunxian [1 ,2 ]
Xia, Jun [1 ,2 ]
Meng, Lin [3 ]
Li, Lingcheng [4 ]
机构
[1] Wuhan Univ, State Key Lab Water Resources & Hydropower Engn S, Wuhan 430072, Peoples R China
[2] Wuhan Univ, Hubei Key Lab Water Syst Sci Sponge City Construc, Wuhan 430072, Peoples R China
[3] Vanderbilt Univ, Dept Earth & Environm Sci, Nashville, TN USA
[4] Pacific Northwest Natl Lab, Atmospher Sci & Global Change Div, Richland, WA 99354 USA
基金
中国国家自然科学基金;
关键词
Land surface phenology; Revegetation; Land use change; Climate change; SOIL ORGANIC-CARBON; SPRING PHENOLOGY; HIGH-LATITUDES; COVER CHANGE; VEGETATION; FORESTS; WATER; FEEDBACKS; TRENDS; TEMPERATURE;
D O I
10.1016/j.scitotenv.2022.160383
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Land surface phenology (LSP), defined as the plant's growth rhythm retrieved from satellite sensing products, is proven to shift with climate change and affect the carbon cycles of terrestrial ecosystems. Global afforested area is largely in-creasing and consequently affecting local and global climate. However, how and to what extent revegetation affects LSP remains relatively unexplored. Here we investigated the difference in four LSPs (i.e., greenup, maturity, senes-cence, and dormancy) and the response of LSP to climate between restored and native vegetation on Loess Plateau, China, where a remarkable process of vegetation restoration happened during 1982-2015. Most study regions showed a longer growing season (LOS) over time, specifically, with a slight delay in greenup but a relatively large delay in se-nescence. We found that air temperature was the dominant factor affecting greenup and maturity, while precipitation mostly controlled the senescence and dormancy in the study area. Under similar climate conditions, the LSP of restored vegetation (i.e., restored forest and grassland) showed a significant difference (p < 0.05) from native ones during 1999-2015. Compared to the native forest, restored forest from cropland and grassland showed a delayed greenup date by 0.3 and 3.6 days (p < 0.05) and an advanced dormancy date of 6.6 and 9.0 days (p < 0.05), respectively. Fur-thermore, the restored vegetation became less sensitive to air temperature than native vegetation, while the restored forest was more sensitive to precipitation, and its growth was affected by the water limitation to a larger extent in the study area. Our study highlights the necessity of considering land use management and its effect on the LSP change to better understand the effect of afforestation on global climate and carbon cycles.
引用
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页数:13
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