The Multiple Perspective Response of Vegetation to Drought on the Qinghai-Tibetan Plateau

• Published in: Remote sensing (Basel, Switzerland) Vol. 15; no. 4; p. 902
• Main Authors: Zhu, Yuying, Zhang, Huamin, Ding, Mingjun, Li, Lanhui, Zhang, Yili
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01.02.2023
• Subjects: China; Climate change; Cold; Comparative analysis; Drought; Droughts; Environmental aspects; Evapotranspiration; Experiments; Grasslands; Growing season; Heterogeneity; High resistance; Humidity; Identification and classification; Measurement; Normalized difference vegetative index; Plant communities; Precipitation; Qinghai-Tibetan Plateau; resistance and resilience; response; Spatial heterogeneity; Stability; Terrestrial ecosystems; Vegetation; Vegetation effects; China; Tibetan Plateau
• ISSN: 2072-4292; 2072-4292
• DOI: 10.3390/rs15040902

The Qinghai-Tibetan Plateau (QTP) is a global center of cold and dry, where the most extensive fragile alpine vegetation exists. Quantitative analysis of drought event characteristics and vegetation response to drought on the QTP is indispensable for understanding the increasing drought events in a warming climate which exacerbate adverse influence on extremely alpine ecosystems. Here, using the standardized precipitation evapotranspiration index (SPEI) and the normalized difference vegetation index (NDVI) from 2000 to 2018, this study analyzed the characteristics of drought events, their temporal impacts, and the stability of vegetation response to drought on the QTP. Results showed that: the characteristics of drought events on the QTP have clear spatial heterogeneity. When compared to the east monsoon region, most of the western regions have higher frequency and lower intensity of drought events. Drought has significant temporal effects on vegetation in grassland areas of the QTP during the growing season, which reach their peak in July and August. The 0–1-month and 3-month time scales were the optimal lagged and accumulated time during the growing season, respectively. The stability of vegetation response to drought showed significant spatial heterogeneity and varied with eco-geographical regions and vegetation types. Generally, forest areas showed high resistance (74.09) and resilience (2.26), followed by crop and grassland areas.