黄河上中游植被动态及其对干湿转换的响应
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国家自然科学基金项目(52079138,52379054)


Vegetation dynamics and its response pattern to dry-wet transition in the upper and middle reaches of the Yellow River
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    摘要:

    利用改进帕尔默干旱指数和标准化降水蒸发指数表征气象干旱,采用土壤水分亏缺指数表征农业干旱,采用线性回归、变点检验以及最大相关系数等方法,明确了黄河上中游不同地理分区植被动态及干旱演变特征,深入探讨了植被对区域干旱演变的响应规律。结果表明:1)1982-2015年流域整体趋于变湿,植被演变和研究区干湿特征于2006年存在突变,表现为由趋于变干转变为趋于变湿;2)2006年后退耕还林力度降低,而年均归一化植被指数由0.006/10a的速率增至0.021/10a(P<0.05),强调了除人类活动外暖湿化进程对黄河上中游植被的加速绿化的重要作用;3)植被对不同干旱类型的响应存在空间异质性,内蒙古高原西部、青藏高原北部和黄土高原北部地区,植被受干旱影响较大,NDVI与干旱指数呈现正相关。研究结果可为黄河流域生态可持续发展提供理论依据和数据支撑。

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    As an essential grain production base in China, environmental changes in the Yellow River Basin directly affect the sustainable development of the basin's economy. The upper and middle reaches are essential for ecological protection and development of the basin in central and western China, and play a key role in maintaining environmental security in northern China. However, frequent drought events seriously threaten the ecological balance and socio-economic development. In this study, we used the self-calibrated Palmer drought severity index and standardized precipitation evaporation index to characterize meteorological drought, and the soil moisture deficit index to characterize agricultural drought. Linear regression, abrupt change point detection, and maximum correlation coefficient methods were used to character the vegetation dynamics and drought evolution characteristics of different geographical divisions in the upper and middle reaches of the Yellow River and further explored the vegetation response to regional drought evolution. Our results showed that: 1) the basin underwent an abrupt change in vegetation evolution and wet-dry transition characteristics in 2006, transitioning from a drier period (1982-2005) to a wetter period (2006-2015).; 2) after 2006, the intensity of reforestation decreased, while the annual average NDVI increased from 0.006/10a to 0.021/10a, emphasizing the important role of the warming-wetting process, in addition to anthropogenic activities, in accelerating the greening of the vegetation in the upper and middle reaches of the Yellow River; 3) there was spatial heterogeneity in the response of vegetation to different drought types. In the western of the Inner Mongolia Plateau, the northern of the Qinghai-Xizang Plateau, and the northern of the Loess Plateau, the vegetation was more affected by drought, and the NDVI showed a positive correlation with the drought index. Compared with agricultural droughts, meteorological droughts had a larger impact range and their impact was further enhanced after 2006. This study can provide a theoretical basis and data support for the ecologically sustainable development of the Yellow River basin.

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程泳铭,刘浏,程湫雅,徐宗学,安强,王宣宣.黄河上中游植被动态及其对干湿转换的响应.生态学报,2025,45(4):1788~1798

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