Time-lag effects of NDVI responses to climate change in the Yamzhog Yumco Basin, South Tibet

Vegetation dynamics and their response to climate change is critical for determining the mechanisms of climate-derived variations in terrestrial ecosystems. Here, the Normalized Difference Vegetation Index (NDVI) and monthly temperature and precipitation data were employed to examine the spatiotempo...

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Bibliographic Details
Main Authors: Zhang, X. (Author), Zhe, M. (Author)
Format: Article
Language:English
Published: Elsevier B.V. 2021
Subjects:
Online Access:View Fulltext in Publisher
LEADER 03213nam a2200529Ia 4500
001 10.1016-j.ecolind.2021.107431
008 220427s2021 CNT 000 0 und d
020 |a 1470160X (ISSN) 
245 1 0 |a Time-lag effects of NDVI responses to climate change in the Yamzhog Yumco Basin, South Tibet 
260 0 |b Elsevier B.V.  |c 2021 
856 |z View Fulltext in Publisher  |u https://doi.org/10.1016/j.ecolind.2021.107431 
520 3 |a Vegetation dynamics and their response to climate change is critical for determining the mechanisms of climate-derived variations in terrestrial ecosystems. Here, the Normalized Difference Vegetation Index (NDVI) and monthly temperature and precipitation data were employed to examine the spatiotemporal patterns in vegetation dynamics and investigate the time-lag effects of vegetation responses to climate variables in the Yamzhog Yumco Basin, South Tibet, during 2000–2018. The results reveal that the annual average growing season NDVI in the basin was 0.28, with lower values in the mountainous regions and higher values broadly distributed in the lake and river zones. An increasing NDVI trend was observed in nearly 62% of the total vegetation area, with significant changes observed in the western and southern boundaries of the basin. The vegetation areas in the eastern part of basin exhibited a decreasing NDVI trend. The growing season NDVI was positively correlated with temperature and precipitation, with temperature being the primary driving factor for vegetation growth across the entire basin. The cumulative temperature and precipitation of the current and previous months had the strongest impact on NDVI variations. The correlation coefficients between the NDVI, and temperature and precipitation were greater than 0.6 in approximately 72% and 60% of the vegetation area, respectively, with Lag 0–1 accounting for most of these larger correlation coefficients. Future development targets for grassland conservation projects, such as the reasonable livestock capacity, should consider the time-lag effects on vegetation dynamics. © 2021 The Authors 
650 0 4 |a Agriculture 
650 0 4 |a China 
650 0 4 |a climate change 
650 0 4 |a Climate change 
650 0 4 |a Climate change 
650 0 4 |a climate variation 
650 0 4 |a Conservation 
650 0 4 |a Conservation projects 
650 0 4 |a conservation status 
650 0 4 |a Correlation coefficient 
650 0 4 |a Development targets 
650 0 4 |a Dynamics 
650 0 4 |a grassland 
650 0 4 |a growing season 
650 0 4 |a growth 
650 0 4 |a livestock farming 
650 0 4 |a mountain region 
650 0 4 |a Mountainous regions 
650 0 4 |a NDVI 
650 0 4 |a NDVI 
650 0 4 |a Normalized difference vegetation index 
650 0 4 |a spatiotemporal analysis 
650 0 4 |a Spatiotemporal patterns 
650 0 4 |a terrestrial ecosystem 
650 0 4 |a Terrestrial ecosystems 
650 0 4 |a Time-lag effects 
650 0 4 |a Vegetation 
650 0 4 |a vegetation dynamics 
650 0 4 |a Vegetation response 
650 0 4 |a Xizang 
650 0 4 |a Xizang 
650 0 4 |a Yamzhog Yumco Basin 
700 1 |a Zhang, X.  |e author 
700 1 |a Zhe, M.  |e author 
773 |t Ecological Indicators