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Regional vegetation dynamics and its response to climate change—a case study in the Tao River Basin in Northwestern China

Bibliographic Data

ID15545704
AuthorsChangbin Li (0000-0001-9239-3304, Lanzhou University, corresponding author), Jiaguo Qi (0000-0002-8183-0297, Zhejiang University), Linshan Yang (0000-0002-6862-4106, Lanzhou University), Shuaibing Wang (0000-0001-7936-3581, Lanzhou University), Wenjin Yang (Lanzhou University), Gaofeng Zhu (0000-0002-3533-9106, Lanzhou University), Songbing Zou (Chinese Academy of Sciences), Feng Zhang (0000-0002-7444-1103, Lanzhou University)
Year2014
Volume9
Issue12
Pages125003-125003
Publication date2014-12-01
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/9/12/125003
OpenAlexW2147651008
LanguageEN
Citations received5
References cited46

The 30-year normalized-difference vegetation index (NDVI) time series from AVHRR/MODIS satellite sensors was used in this study to assess the regional vegetation dynamic changes in the Tao River Basin, which cuts across the Eastern Tibetan Plateau (ETP) and the Southwestern Loess Plateau (SLP). First, principal component and correlation analyses were carried out to determine the key climatic variables driving ecological change in the region. Then, regression models were tested to correlate NDVI with the selected climatic variables to determine their predictive power. Finally, Sen's slope method was used to determine how terrestrial vegetation has responded to regional climate change in the region. The results indicated an average winter season NDVI value of 0.14 in the ETP but only 0.04 in the SLP. Primarily driven by increasing temperature, vegetation growth has generally been enhanced since 1981; spring NDVI increased by 0.03 every 10 years in the ETP and 0.02 in the SLP. Further, results from trend analyses suggest vegetation growth in the ETP shifted to earlier-start and earlier-end dates, however in the SLP, the growing season has been extended with an earlier-start and later-end date. The precipitation threshold for vegetation germination, measured by the cumulative spring rainfall, was found to be 44 mm for both the ETP and SLP

Climate change · Climatology · Geography · Growing season · Loess plateau · Meteorology · Normalized Difference Vegetation Index · Physical geography · Plateau (mathematics · Precipitation · Structural basin · Vegetation (pathology · Ecology and Vegetation Dynamics Studies · Environmental Science · Plant Water Relations and Carbon Dynamics · Remote Sensing in Agriculture · Ecology · Geology · Soil Science

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Citations per year0.38
Citation span2013 - 2022 (10)
Highly citedNo

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