Wind Speed and Vegetation Coverage in Turn Dominated Wind Erosion Change With Increasing Aridity in Africa

IF 7.3 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Earths Future Pub Date : 2024-06-10 DOI:10.1029/2024EF004468
Hanbing Zhang, Jian Peng, Chaonan Zhao
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Abstract

Wind erosion is one of the main causes of land degradation and desertification. Clarifying the spatiotemporal variations of wind erosion and the dominant factors of its spatial characteristics and the temporal trend will contribute to the establishment of appropriate wind erosion control and management practices, which is essential for combating global land degradation and strengthening ecological protection in drylands. Here, we assessed wind erosion in Africa during 2001–2020 based on the Revised Wind Erosion Equation (RWEQ). We also analyzed the influential factor of spatial characteristics and temporal variation based on machine learning and other methods under different aridity. Results revealed that the average annual wind erosion modulus was 16,672 t/km2/a in Africa during 2001–2020, with hyper-arid areas and arid areas accounting for more than 90% of the total wind erosion modulus. The spatial characteristics of wind erosion were dominated by natural factors but not anthropogenic activities. Except in hyper-arid areas, wind speed and vegetation coverage together dominated the spatial characteristics. Wind speed was the dominant factor in wind erosion change, while in arid and semi-arid areas, the capability of vegetation coverage to affect wind erosion change was comparable to wind speed. It can be concluded that, although revegetation does contribute to the reduction of wind erosion in arid and semi-arid areas, taking into account water resource constraints and land use conflicts, large plantations can be replaced with windbreaks to increase vegetation coverage while reducing near-surface wind speed, which improves the sustainability of ecological projects aimed at combating land degradation and desertification.

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风速和植被覆盖率在转折主导的风蚀作用下随着非洲日益干旱而变化
风蚀是造成土地退化和荒漠化的主要原因之一。厘清风蚀的时空变化及其空间特征和时间趋势的主导因素,将有助于建立适当的风蚀控制和管理方法,这对于应对全球土地退化和加强旱地生态保护至关重要。在此,我们根据修订的风蚀方程(RWEQ)评估了 2001-2020 年间非洲的风蚀情况。我们还基于机器学习等方法分析了不同干旱度下空间特征和时间变化的影响因素。结果表明,2001-2020年间,非洲年均风蚀模量为16672 t/km2/a,其中超干旱区和干旱区的风蚀模量占总风蚀模量的90%以上。风蚀的空间特征以自然因素为主,而非人为活动。除超干旱区外,风速和植被覆盖度共同主导了风蚀的空间特征。风速是风蚀变化的主导因素,而在干旱和半干旱地区,植被覆盖对风蚀变化的影响能力与风速相当。由此可以得出结论,尽管在干旱和半干旱地区,植被重建确实有助于减少风蚀,但考虑到水资源的限制和土地利用的冲突,可以用防风林取代大面积种植,以增加植被覆盖率,同时降低近地面风速,从而提高旨在防治土地退化和荒漠化的生态项目的可持续性。
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来源期刊
Earths Future
Earths Future ENVIRONMENTAL SCIENCESGEOSCIENCES, MULTIDI-GEOSCIENCES, MULTIDISCIPLINARY
CiteScore
11.00
自引率
7.30%
发文量
260
审稿时长
16 weeks
期刊介绍: Earth’s Future: A transdisciplinary open access journal, Earth’s Future focuses on the state of the Earth and the prediction of the planet’s future. By publishing peer-reviewed articles as well as editorials, essays, reviews, and commentaries, this journal will be the preeminent scholarly resource on the Anthropocene. It will also help assess the risks and opportunities associated with environmental changes and challenges.
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