Abstract
This chapter describes the spatial distribution of aeolian desertification and its temporal change in northern China and Mongolia using remote sensing images and the aeolian desertification index. In northern China, aeolian desertification mainly occurs in semiarid and subhumid agropastoral ecotones, arid and semiarid pure pastoral regions, and arid oases in inland river basins. The area of aeolian desertification in northern China rapidly increased from 13.7 × 104 km2 in the 1950s to 38.6 × 104 km2 in 2000 and then slowly decreased to 37.6 × 104 km2 in the 2010s. Human activities are the main driving forces of aeolian desertification and its restoration in northern China. Aeolian sands cover approximately 2% of the total territory of Mongolia and are distributed through aeolian processes. In terms of aeolian desertification, the latest studies indicate that approximately 68% of degraded lands are caused by wind erosion, i.e., deflation, transportation, and accumulation of sand. Aeolian desertification is mainly linked to the rapid decline in vegetation cover, decreases in surface roughness, and increases in the aridity of the climate.
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Wang, T., Nyamtseren, M. (2022). Spatial Distribution and Temporal Dynamics of Aeolian Desertification. In: Wang, T., Tsunekawa, A., Xue, X., Kurosaki, Y. (eds) Combating Aeolian Desertification in Northeast Asia. Ecological Research Monographs. Springer, Singapore. https://doi.org/10.1007/978-981-16-9028-0_3
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