Impacts of climate change on vegetation phenology and net primary productivity in arid Central Asia

物候学 环境科学 归一化差异植被指数 气候变化 增强植被指数 初级生产 干旱 生产力 植被(病理学) 热带植被 自然地理学 地理 气候学 降水 生长季节 生态系统 生态学 植被指数 热带 气象学 地质学 生物 宏观经济学 病理 经济 医学
作者
Lizhou Wu,Xiaofei Ma,Xin Dou,Jianting Zhu,Chengyi Zhao
出处
期刊:Science of The Total Environment [Elsevier]
卷期号:796: 149055-149055 被引量:122
标识
DOI:10.1016/j.scitotenv.2021.149055
摘要

Vegetation is highly sensitive to climate changes in arid regions. The relationship between vegetation and climate changes can be effectively characterized by vegetation phenology. However, few studies have examined the vegetation phenology and productivity changes in arid Central Asia (ACA). The vegetation phenological information of ACA was extracted using MODIS NDVI (Normalized Difference Vegetation Index) data, and the dynamics of vegetation phenological changes under spatiotemporal variations were quantitatively assessed. Moreover, the impacts of climate change on vegetation phenology and net primary productivity were analyzed by combining meteorological data with that of MODIS NPP (Net Primary Productivity) during the same period. The results demonstrated that the start of the season (SOS) of vegetation in the study was concentrated from mid-February to mid-April, while the end of the season (EOS) was concentrated from early October to mid-December. The length of growing season (LOS) ranged from 6 to 10 months. The SOS of vegetation was gradually postponed at a rate of 0.16 d·year−1. The EOS advanced at a rate of 0.69 d·year−1. The LOS was gradually shortened at a rate of 0.89 d·year−1. For each per 1000 m increase in elevation, the SOS of vegetation was postponed by 12.40 d; the EOS advanced by 0.40 d, and the LOS was shortened by 11.70 d. For the impacts of climate changes on vegetation phenology and NPP, the SOS of vegetation phenology negatively correlated with temperature but positively correlated with precipitation and NPP. The EOS and LOS positively correlated with temperature but negatively with precipitation and NPP. Results indicated that the SOS was not moved ahead but was delayed, while the EOS advanced rather than being postponed under climate change. These results can offer new insights on the phenological response to climate change in arid regions and on non-systematic changes in phenology under global warming.

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