Divergent climatic effects on forest greenness modulated by temperature and precipitation gradients in the Yellow River Basin, China

被引:0
|
作者
Tao, Jian [1 ]
Xu, Yuqian [1 ]
Cong, Nan [2 ]
Li, Chanjuan [3 ]
Zhao, Guangshuai [4 ]
Miao, Chenglin [3 ]
机构
[1] Shandong Technol & Business Univ, Coll Publ Adm, Yantai 264005, Peoples R China
[2] Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Ecosyst Network Observat & Modeling, Nagqu Alpine Grassland Res Stn, Beijing 100101, Peoples R China
[3] Shandong Technol & Business Univ, Sch Management, Yantai 264005, Peoples R China
[4] Natl Forestry & Grassland Adm, Dev Res Ctr, Beijing 100714, Peoples R China
关键词
Forest greenness; Leaf area index; Water resource limitation; Climate warming; LOESS PLATEAU; WATER-RESOURCE; VEGETATION; RESPONSES; EVAPOTRANSPIRATION; GROWTH; TREND;
D O I
10.1016/j.ecolind.2024.111553
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
How climatic effects on forest greenness vary between different temperature and precipitation gradients in climate-sensitive and ecologically fragile areas, such as the Yellow River Basin (YRB) in China, is not well understood. Here we used meteorological data and remotely sensed leaf area index (LAI) data to investigate climatic effects on forest LAI changes along temperature-precipitation gradients in the YRB from 2001 to 2020. We found that changing precipitation thresholds divided forests into higher and lower LAI areas. The precipitation thresholds increased from 400 mm mean annual precipitation (MAP) in areas with a mean annual temperature (MAT) below 4 degrees C to 500 mm MAP in areas with a MAT above 4 degrees C. Forest LAI increased significantly from 2001 to 2020. The MAT and MAP thresholds changed when dividing forests into different areas with different LAI values and climatic effects. Forests greening was mainly driven by temperature in areas with LAI values between 3 and 6 m2 m- 2 but was mainly driven by precipitation in areas with LAI values less than 3 m2 m- 2. The threshold of MAP isopleth increased from 500 mm to 700 mm and then decreased to 500 mm, while the MAT increased from less than 0 degrees C to 5 degrees C and then increased to 12 degrees C. These divergent climatic effects were caused by the combined effects of water resource limitations and increasing evapotranspiration. Identifying MAT and MAP thresholds is helpful for decision-maker and managers to optimize forest restoration more accurately in future ecological protection projects facing the challenge of limited water resources in the YRB.
引用
收藏
页数:10
相关论文
共 50 条
  • [31] Potential effects of climate change on runoff in the Yellow River basin of China
    Zhang, G.-H.
    Fu, S.-H.
    Fang, W.-H.
    Imura, H.
    Zhang, X.-C.
    TRANSACTIONS OF THE ASABE, 2007, 50 (03) : 911 - 918
  • [32] Response of Soil Moisture to Hydro-meteorological Variables Under Different Precipitation Gradients in the Yellow River Basin
    Li, Sha
    Liang, Wei
    Zhang, Weibin
    Liu, Qinghua
    WATER RESOURCES MANAGEMENT, 2016, 30 (06) : 1867 - 1884
  • [33] Influence of Precipitation Effects Induced by Large-Scale Irrigation in Northwest China on Soil Erosion in the Yellow River Basin
    Huang, Ya
    Zhao, Yong
    Li, Guiping
    Yang, Jing
    Li, Yanping
    REMOTE SENSING, 2023, 15 (07)
  • [34] Response of Soil Moisture to Hydro-meteorological Variables Under Different Precipitation Gradients in the Yellow River Basin
    Sha Li
    Wei Liang
    Weibin Zhang
    Qinghua Liu
    Water Resources Management, 2016, 30 : 1867 - 1884
  • [35] Magnitude and Frequency of Temperature and Precipitation Extremes and the Associated Atmospheric Circulation Patterns in the Yellow River Basin (1960-2017), China
    Dong, Xiaogang
    Zhang, Shiting
    Zhou, Junju
    Cao, Jianjun
    Jiao, Liang
    Zhang, Zhiyang
    Liu, Yang
    WATER, 2019, 11 (11)
  • [36] Dipolar mode of summer precipitation over the Upper Yellow River Basin in China and possible causes
    Zhang, Jinyu
    Yue, Ping
    Zhao, Jianhua
    Yang, Yang
    THEORETICAL AND APPLIED CLIMATOLOGY, 2024, 155 (6) : 5093 - 5105
  • [37] Trends in precipitation extremes over the Yellow River basin in North China: Changing properties and causes
    Gao, Tao
    Wang, Huailiang
    HYDROLOGICAL PROCESSES, 2017, 31 (13) : 2412 - 2428
  • [38] Spatio-temporal evolutions of precipitation in the Yellow River basin of China from 1981 to 2013
    Wu, Lei
    Liu, Xia
    Ma, Xiaoyi
    WATER SCIENCE AND TECHNOLOGY-WATER SUPPLY, 2016, 16 (05): : 1441 - 1450
  • [39] Deterministic and probabilistic projections and their credibility in analyzing future precipitation variations in the Yellow River Basin, China
    Sun, Zhouliang
    Liu, Yanli
    Zhang, Jianyun
    Chen, Hua
    Shu, Zhangkang
    Guan, Tiesheng
    Wang, Guoqing
    Jin, Junliang
    Bao, Zhenxin
    Liu, Cuishan
    JOURNAL OF WATER AND CLIMATE CHANGE, 2022, 13 (04) : 1806 - 1829
  • [40] Coupling Effects of Precipitation and Vegetation on Sediment Yield from the Perspective of Spatiotemporal Heterogeneity across the Qingshui River Basin of the Upper Yellow River, China
    Yang, Jun
    Zhang, Huilan
    Yang, Weiqing
    FORESTS, 2022, 13 (03):