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Identifying land restoration regions and their driving mechanisms in inner Mongolia, China from 1981 to 2010

机译:识别1981年至2010年中国内蒙古的土地恢复区及其驱动机制

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Land degradation is a global environmental issue and efforts to achieve land restoration call for urgent action. This study selected Inner Mongolia of China as a research area and assessed the relative contribution of climate variability and human activities affecting land restoration during different time intervals from 1981 to 2010. The results showed that the spatial extent of land restoration in Inner Mongolia has increased significantly from 1981 to 2010, to more than 248,512 km(2), accounting for 2.11% of the total area. Climatic factors showed heterogeneity in different time intervals; temperature and sunshine duration were the main factors induced land restoration from 1981 to 1995, which mainly attributed to its' positive effect on promoting vegetation photosynthetic efficiency; however, the decrease in wind speed played the most important role in land restoration from 1996 to 2010. The land restoration areas have also been closely associated with human activities, particularly from 1996 to 2010, when afforestation was the main factor driving the increase of land restoration areas, showing that the implementation of the ecological restoration policy of China has played a positive role in land conservation. In addition, the mutual impacts of climate variability and human activities on land restoration have been observed at different scales.
机译:土地退化是一个全球性的环境问题,为实现土地恢复而做出的努力需要采取紧急行动。本研究选择了中国内蒙古作为研究区域,并评估了1981年至2010年不同时间间隔内气候变化和人类活动对土地恢复的相对贡献。结果表明,内蒙古土地恢复的空间范围显着增加从1981年到2010年,超过248,512 km(2),占总面积的2.11%。气候因素在不同的时间间隔表现出异质性。 1981年至1995年,气温和日照时间是引起土地恢复的主要因素,主要归因于其对促进植被光合效率的积极作用。然而,从1996年至2010年,风速的降低在土地恢复中起着最重要的作用。土地恢复区也与人类活动密切相关,尤其是从1996年至2010年,植树造林是推动土地增加的主要因素恢复区,说明中国生态恢复政策的实施对土地保护起到了积极作用。此外,还观察到了不同程度的气候变化和人类活动对土地恢复的相互影响。

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