School of Geography and Tourism, Chongqing Normal University, No. 37, Daxuecheng Middle Road, Shapingba District, Chongqing, 401331, China.
Chongqing Key Laboratory of Geographic Information System Application, Chongqing, 401331, China.
Environ Sci Pollut Res Int. 2023 Dec;30(59):123259-123273. doi: 10.1007/s11356-023-30920-y. Epub 2023 Nov 20.
Karst desertification (KD) is a unique desert ecological phenomenon occurring in the karst region of Southwest China (KRSC). Studying the KD evolution process and distinguishing the influences of human activities and climate factors on KD are essential for restoring KD areas. This article is based on MODIS remote sensing data and ERA5-Land data. Additionally, multiple linear regression models, correlation analysis, and residual analysis are utilized to analyze the spatiotemporal evolution characteristics of KD in the southwest region of China from 2000 to 2020. This study aims to differentiate the impacts of human activities and climate change on the desertification process in karst areas. (1) In the southwest region of China, the overall KD shows an intensifying trend at both ends of the study area and an ameliorating distribution pattern in the central region. In particular, Guizhou province, which is located in the center of the study area, demonstrated significant suppression in the KD process from 2000 to 2020. (2) In the southwest karst region, there are significant spatial differences in the correlation between the KD process and precipitation, temperature, and radiation. Temperature is significantly negatively correlated in most parts of Yunnan. (3) According to the residual analysis, approximately 89.62% of the karst areas in the southwest are influenced by climate, while 10.38% are influenced by human activities. Climate change has a relatively small impact on the ability to improve KD compared to the disruptive influence of human activities. Some human activities, such as afforestation, in which grassland and cultivated land are converted to forest, play a substantial role in inhibiting the KD process. Conversely, the rapid expansion of urban areas tends to exacerbate KD in adjacent regions. Therefore, this study of the evolution process of KD in Southwest China can provide a scientific basis for monitoring and controlling KD and provide theoretical support for coping with the challenges posed by KD to China's ecological environment.
喀斯特荒漠化(KD)是中国西南喀斯特地区特有的荒漠生态现象。研究 KD 演化过程,区分人类活动和气候因素对 KD 的影响,对于恢复 KD 地区至关重要。本文基于 MODIS 遥感数据和 ERA5-Land 数据,利用多元线性回归模型、相关分析和残差分析方法,分析了 2000-2020 年中国西南地区 KD 的时空演化特征,旨在区分人类活动和气候变化对喀斯特地区荒漠化过程的影响。(1)中国西南地区整体 KD 呈两端增强、中部改善的分布格局。特别是研究区中心的贵州省,2000-2020 年 KD 过程得到了显著抑制。(2)西南喀斯特地区 KD 过程与降水、温度和辐射的相关性存在显著的空间差异。云南大部分地区温度呈显著负相关。(3)根据残差分析,西南喀斯特地区约 89.62%的地区受到气候的影响,10.38%的地区受到人类活动的影响。气候变化对改善 KD 的能力影响相对较小,而人类活动的干扰影响较大。一些人类活动,如将草地和耕地转化为森林的造林,在抑制 KD 过程中发挥了重要作用。相反,城市面积的快速扩张往往会加剧邻近地区的 KD。因此,本研究对中国西南地区 KD 演化过程的研究,可以为监测和控制 KD 提供科学依据,为应对 KD 对中国生态环境的挑战提供理论支持。