Spatiotemporal dynamics and drivers of wind erosion on the Qinghai-Tibet Plateau, China

Land degradation caused by wind erosion seriously threatens the supply of ecosystem services on the Qinghai-Tibet Plateau (QTP). Assessing wind erosion variations is critical to identify key change areas and formulate desertification control strategies. In this study, we evaluated the spatiotemporal...

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Autores principales: Yanmin Teng, Jinyan Zhan, Wei Liu, Yongxiu Sun, Frank Boappeah Agyemang, Li Liang, Zhihui Li
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Publicado: Elsevier 2021
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spelling oai:doaj.org-article:fdf3c63663ba447894f2c0a2b45f034b2021-12-01T04:43:20ZSpatiotemporal dynamics and drivers of wind erosion on the Qinghai-Tibet Plateau, China1470-160X10.1016/j.ecolind.2021.107340https://doaj.org/article/fdf3c63663ba447894f2c0a2b45f034b2021-04-01T00:00:00Zhttp://www.sciencedirect.com/science/article/pii/S1470160X21000054https://doaj.org/toc/1470-160XLand degradation caused by wind erosion seriously threatens the supply of ecosystem services on the Qinghai-Tibet Plateau (QTP). Assessing wind erosion variations is critical to identify key change areas and formulate desertification control strategies. In this study, we evaluated the spatiotemporal dynamics in wind erosion on the QTP from 1980 to 2015 using the Revised Wind Erosion Equation (RWEQ). Furthermore, we analysed the spatial correlation between wind erosion dynamics, climate change and human activities and identified the main driving factors. The results showed that wind erosion intensity on the QTP increased continuously from southeast to northwest. Areas with moderate or high soil erosion intensity (>25 t·hm−2·a−1), accounting for 53.48% of the region, were mostly distributed on the western and northern areas of the plateau. The mean annual soil wind erosion modulus (SWEM) of the entire region during 1980–2015 was 32.08 t·hm−2·a−1, with an evident decline at a rate of approximately 0.14 t·hm−2·a−1 in this period. However, wind erosion increased significantly in 9.99% of the QTP, mainly in the northwestern part of the region. Areas with significant changes in wind erosion driven by climate change and human activities accounted for 54.74% and 18.89% of the plateau, respectively. The influence of climate change on wind erosion is characterized by large scale and spatial continuity, while the impact of human activities on wind erosion occurs in local areas and distributes in patches. This study has implications for spatially revealing the climate and human drivers of wind erosion changes and identifying pivotal zones for desertification prevention on the QTP.Yanmin TengJinyan ZhanWei LiuYongxiu SunFrank Boappeah AgyemangLi LiangZhihui LiElsevierarticleSoil erosionRWEQClimate changeHuman activitiesLand degradation, Qinghai-Tibetan PlateauEcologyQH540-549.5ENEcological Indicators, Vol 123, Iss , Pp 107340- (2021)
institution DOAJ
collection DOAJ
language EN
topic Soil erosion
RWEQ
Climate change
Human activities
Land degradation, Qinghai-Tibetan Plateau
Ecology
QH540-549.5
spellingShingle Soil erosion
RWEQ
Climate change
Human activities
Land degradation, Qinghai-Tibetan Plateau
Ecology
QH540-549.5
Yanmin Teng
Jinyan Zhan
Wei Liu
Yongxiu Sun
Frank Boappeah Agyemang
Li Liang
Zhihui Li
Spatiotemporal dynamics and drivers of wind erosion on the Qinghai-Tibet Plateau, China
description Land degradation caused by wind erosion seriously threatens the supply of ecosystem services on the Qinghai-Tibet Plateau (QTP). Assessing wind erosion variations is critical to identify key change areas and formulate desertification control strategies. In this study, we evaluated the spatiotemporal dynamics in wind erosion on the QTP from 1980 to 2015 using the Revised Wind Erosion Equation (RWEQ). Furthermore, we analysed the spatial correlation between wind erosion dynamics, climate change and human activities and identified the main driving factors. The results showed that wind erosion intensity on the QTP increased continuously from southeast to northwest. Areas with moderate or high soil erosion intensity (>25 t·hm−2·a−1), accounting for 53.48% of the region, were mostly distributed on the western and northern areas of the plateau. The mean annual soil wind erosion modulus (SWEM) of the entire region during 1980–2015 was 32.08 t·hm−2·a−1, with an evident decline at a rate of approximately 0.14 t·hm−2·a−1 in this period. However, wind erosion increased significantly in 9.99% of the QTP, mainly in the northwestern part of the region. Areas with significant changes in wind erosion driven by climate change and human activities accounted for 54.74% and 18.89% of the plateau, respectively. The influence of climate change on wind erosion is characterized by large scale and spatial continuity, while the impact of human activities on wind erosion occurs in local areas and distributes in patches. This study has implications for spatially revealing the climate and human drivers of wind erosion changes and identifying pivotal zones for desertification prevention on the QTP.
format article
author Yanmin Teng
Jinyan Zhan
Wei Liu
Yongxiu Sun
Frank Boappeah Agyemang
Li Liang
Zhihui Li
author_facet Yanmin Teng
Jinyan Zhan
Wei Liu
Yongxiu Sun
Frank Boappeah Agyemang
Li Liang
Zhihui Li
author_sort Yanmin Teng
title Spatiotemporal dynamics and drivers of wind erosion on the Qinghai-Tibet Plateau, China
title_short Spatiotemporal dynamics and drivers of wind erosion on the Qinghai-Tibet Plateau, China
title_full Spatiotemporal dynamics and drivers of wind erosion on the Qinghai-Tibet Plateau, China
title_fullStr Spatiotemporal dynamics and drivers of wind erosion on the Qinghai-Tibet Plateau, China
title_full_unstemmed Spatiotemporal dynamics and drivers of wind erosion on the Qinghai-Tibet Plateau, China
title_sort spatiotemporal dynamics and drivers of wind erosion on the qinghai-tibet plateau, china
publisher Elsevier
publishDate 2021
url https://doaj.org/article/fdf3c63663ba447894f2c0a2b45f034b
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