Response of grassland NDVI change velocity to climate velocity in the alpine mountainous region

• QLMs grassland NDVI GS velocity exceeds temperature (54.1% areas) but trails precipitation (77.8%), showing precipitation dominance. • Steep slopes slow climate velocities, enhancing refugia; flat terrains face higher adaptation pressures. • Alpine grasslands show asymmetric responses to multi-climate velocities, requiring temperature-precipitation synergy for management. Under climate warming, grassland vegetation in mountainous regions responds rapidly to climate change but often lags behind the rate of climatic shifts. The Qilian Mountains (QLMs), a representative alpine mountainous area, have experienced a warming rate significantly exceeding the global average. However, whether the change velocity of grassland NDVI in the QLMs matches climate velocity remains unclear, and there is an urgent need to determine if regional grasslands can adapt to the “velocity race” driven by climate change. To address this gap, this study analyzed the spatiotemporal trends of change velocities in growing-season grassland NDVI (NDVI GS ), temperature, and precipitation across the QLMs using the local climate velocity method combined with a moving window technique. Results showed that from 2000 to 2024, the velocities of grassland NDVI GS , temperature, and precipitation all increased, with precipitation velocity exhibiting the fastest growth rate. Their mean values were 0.08 ± 0.08 km·a −1 (NDVI GS ), 0.07 ± 0.07 km·a −1 (temperature), and 0.24 ± 0.26 km·a −1 (precipitation), indicating that grassland NDVI GS velocity was intermediate between temperature and precipitation velocities. Spatially, 54.1 % of grassland areas displayed NDVI GS velocities exceeding temperature velocities, while 77.8 % of areas showed NDVI GS velocities lower than precipitation velocities. In conclusion, the response of grassland NDVI GS velocity to temperature and precipitation velocities exhibits regional heterogeneity. These findings provide important scientific insights for guiding grassland restoration and adaptive management in alpine mountainous regions.

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Publication Details

Journal
Ecological Indicators
Published
2025-09-04
DOI
https://doi.org/10.1016/j.ecolind.2025.114153
Citations
1
Primary Topic
Tree-ring climate responses
Type
article
Field-Weighted Citation Impact
1.30
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article

Response of grassland NDVI change velocity to climate velocity in the alpine mountainous region

Zhilan Wang, Qingyu Guan, Qinqin Du, Mingjun Zhang et al.
1 citations
Ecological Indicators
Tree-ring climate responses
1.30
article

Response of grassland NDVI change velocity to climate velocity in the alpine mountainous region

Zhilan Wang, Qingyu Guan, Qinqin Du, Mingjun Zhang, Yunfan Sun
article en
1 citations

Abstract

• QLMs grassland NDVI GS velocity exceeds temperature (54.1% areas) but trails precipitation (77.8%), showing precipitation dominance. • Steep slopes slow climate velocities, enhancing refugia; flat terrains face higher adaptation pressures. • Alpine grasslands show asymmetric responses to multi-climate velocities, requiring temperature-precipitation synergy for management. Under climate warming, grassland vegetation in mountainous regions responds rapidly to climate change but often lags behind the rate of climatic shifts. The Qilian Mountains (QLMs), a representative alpine mountainous area, have experienced a warming rate significantly exceeding the global average. However, whether the change velocity of grassland NDVI in the QLMs matches climate velocity remains unclear, and there is an urgent need to determine if regional grasslands can adapt to the “velocity race” driven by climate change. To address this gap, this study analyzed the spatiotemporal trends of change velocities in growing-season grassland NDVI (NDVI GS ), temperature, and precipitation across the QLMs using the local climate velocity method combined with a moving window technique. Results showed that from 2000 to 2024, the velocities of grassland NDVI GS , temperature, and precipitation all increased, with precipitation velocity exhibiting the fastest growth rate. Their mean values were 0.08 ± 0.08 km·a −1 (NDVI GS ), 0.07 ± 0.07 km·a −1 (temperature), and 0.24 ± 0.26 km·a −1 (precipitation), indicating that grassland NDVI GS velocity was intermediate between temperature and precipitation velocities. Spatially, 54.1 % of grassland areas displayed NDVI GS velocities exceeding temperature velocities, while 77.8 % of areas showed NDVI GS velocities lower than precipitation velocities. In conclusion, the response of grassland NDVI GS velocity to temperature and precipitation velocities exhibits regional heterogeneity. These findings provide important scientific insights for guiding grassland restoration and adaptive management in alpine mountainous regions.

Ecological IndicatorsVol. 179
Northwest Normal University (CN), Lanzhou University (CN)
Openalex Percentile: Top 18%
Tree-ring climate responses
1.30
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