Characteristics of spatial and temporal dynamics of vegetation and its response to climate extremes in ecologically fragile and climate change sensitive areas – A case study of Hexi region
[Display omitted] •NDVI shows an overall increasing trend from 2000 to 2020.•The Hexi region shows a warming and wetting trend.•Extreme precipitation is more important for NDVI.•The lag effect of NDVI on climate extremes varies by indicators and spaces. Climate extremes significantly affects vegetat...
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Veröffentlicht in: | Catena (Giessen) 2024-04, Vol.239, p.107910, Article 107910 |
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Sprache: | eng |
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•NDVI shows an overall increasing trend from 2000 to 2020.•The Hexi region shows a warming and wetting trend.•Extreme precipitation is more important for NDVI.•The lag effect of NDVI on climate extremes varies by indicators and spaces.
Climate extremes significantly affects vegetation dynamics, and understanding the relationship between dryland vegetation and climate extremes is crucial for regional ecological security and disaster warning. According to meteorological and satellite remote sensing data, the paper analyses the dynamics of normalized difference vegetation index (NDVI) and climate extremes in the Hexi region from 2000 to 2020 using Theil-Sen Median, Mann-Kendall and linear regression methods; the relationship between climate extremes and vegetation dynamics is revealed using Pearson correlation and boosted regression trees (BRT) models. On this basis, the time-lag effect of NDVI in response to climate extremes was further investigated. The results show that the NDVI in the Hexi region increased from 2000 to 2020, with significant greening (67.72 %) and a small amount of degradation concentrated in the desert in the northwest and the oasis in the southeast. The correlation between climate extremes indicators and NDVI shows a large spatial heterogeneity, with extreme precipitation showing a high importance for all regions except oasis. NDVI has no lag or 1 month lag for extreme temperature, no lag for max 1-day precipitation amount (Rx1day) for areas other than mountainous areas, and a 3-month lag for max 5-day precipitation amount (Rx5day) for extensive areas. The results of this study could serve as a reference for the study of the relationship between vegetation dynamics and climate extremes in arid and semi-arid regions, and provide a theoretical basis for the establishment of scientific and reasonable strategies for regional vegetation restoration and conservation. |
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ISSN: | 0341-8162 1872-6887 |
DOI: | 10.1016/j.catena.2024.107910 |