Impact ways and their contributions to vegetation-induced runoff changes in the Loess Plateau
Study region: Sixteen typical watersheds with long-term continuous runoff monitoring within the Loess Plateau (100°54′∼114°33′E, 33°43′∼41°16′N), Northwest China. Study focus: Focusing on the period before and after implementing China's ''Grain-for-Green'' Program (GFGP) (st...
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Elsevier
2024-02-01
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Series: | Journal of Hydrology: Regional Studies |
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Online Access: | http://www.sciencedirect.com/science/article/pii/S2214581823003178 |
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author | Xingyan Tan Yangwen Jia Dawen Yang Cunwen Niu Chunfeng Hao |
author_facet | Xingyan Tan Yangwen Jia Dawen Yang Cunwen Niu Chunfeng Hao |
author_sort | Xingyan Tan |
collection | DOAJ |
description | Study region: Sixteen typical watersheds with long-term continuous runoff monitoring within the Loess Plateau (100°54′∼114°33′E, 33°43′∼41°16′N), Northwest China. Study focus: Focusing on the period before and after implementing China's ''Grain-for-Green'' Program (GFGP) (started in 1999), this study analyzed runoff and vegetation changes and how the latter affects the former. New hydrological insights for the region: The results show that the vegetation change effect was the main driver of runoff reduction over the LP from 1982–1999 to 2000–2015 and accounted for 78.94% (59.71–97.25%) of the reduced runoff. Changes in vegetation under multiple anthropogenic and natural influences are mainly characterized by increases in greenness, growing season length, and woodland and grassland area (along with a decrease in cultivated area). These changes have altered the repartition of precipitation in favor of evapotranspiration rather than runoff. The GFGP-led LULC shift, particularly the reduction of cropland, plays a vital role (GRD > 0.80) in vegetation-induced runoff losses, which may exacerbate future water stress in the region. To curb the LP's continuous attenuation of river runoff and promote the Yellow River Basin's ecological protection and high-quality development, we suggest focusing on the vegetation change effects on runoff and optimizing afforestation measures. |
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language | English |
last_indexed | 2024-03-08T10:29:54Z |
publishDate | 2024-02-01 |
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series | Journal of Hydrology: Regional Studies |
spelling | doaj.art-cf1ab3fb581f40978ece54b6b69e6a222024-01-27T06:55:01ZengElsevierJournal of Hydrology: Regional Studies2214-58182024-02-0151101630Impact ways and their contributions to vegetation-induced runoff changes in the Loess PlateauXingyan Tan0Yangwen Jia1Dawen Yang2Cunwen Niu3Chunfeng Hao4State Key Laboratory of Hydroscience and Engineering, Department of Hydraulic Engineering, Tsinghua University, Beijing 100084, China; State Key Laboratory of Simulation and Regulation of River Basin Water Cycle (SKL-WAC), China Institute of Water Resources and Hydropower Research (IWHR), Beijing 100038, ChinaState Key Laboratory of Simulation and Regulation of River Basin Water Cycle (SKL-WAC), China Institute of Water Resources and Hydropower Research (IWHR), Beijing 100038, China; Corresponding author.State Key Laboratory of Hydroscience and Engineering, Department of Hydraulic Engineering, Tsinghua University, Beijing 100084, ChinaState Key Laboratory of Simulation and Regulation of River Basin Water Cycle (SKL-WAC), China Institute of Water Resources and Hydropower Research (IWHR), Beijing 100038, ChinaState Key Laboratory of Simulation and Regulation of River Basin Water Cycle (SKL-WAC), China Institute of Water Resources and Hydropower Research (IWHR), Beijing 100038, ChinaStudy region: Sixteen typical watersheds with long-term continuous runoff monitoring within the Loess Plateau (100°54′∼114°33′E, 33°43′∼41°16′N), Northwest China. Study focus: Focusing on the period before and after implementing China's ''Grain-for-Green'' Program (GFGP) (started in 1999), this study analyzed runoff and vegetation changes and how the latter affects the former. New hydrological insights for the region: The results show that the vegetation change effect was the main driver of runoff reduction over the LP from 1982–1999 to 2000–2015 and accounted for 78.94% (59.71–97.25%) of the reduced runoff. Changes in vegetation under multiple anthropogenic and natural influences are mainly characterized by increases in greenness, growing season length, and woodland and grassland area (along with a decrease in cultivated area). These changes have altered the repartition of precipitation in favor of evapotranspiration rather than runoff. The GFGP-led LULC shift, particularly the reduction of cropland, plays a vital role (GRD > 0.80) in vegetation-induced runoff losses, which may exacerbate future water stress in the region. To curb the LP's continuous attenuation of river runoff and promote the Yellow River Basin's ecological protection and high-quality development, we suggest focusing on the vegetation change effects on runoff and optimizing afforestation measures.http://www.sciencedirect.com/science/article/pii/S2214581823003178Runoff changeBudyko attribution analysisVegetation variationThe Loess Plateau |
spellingShingle | Xingyan Tan Yangwen Jia Dawen Yang Cunwen Niu Chunfeng Hao Impact ways and their contributions to vegetation-induced runoff changes in the Loess Plateau Journal of Hydrology: Regional Studies Runoff change Budyko attribution analysis Vegetation variation The Loess Plateau |
title | Impact ways and their contributions to vegetation-induced runoff changes in the Loess Plateau |
title_full | Impact ways and their contributions to vegetation-induced runoff changes in the Loess Plateau |
title_fullStr | Impact ways and their contributions to vegetation-induced runoff changes in the Loess Plateau |
title_full_unstemmed | Impact ways and their contributions to vegetation-induced runoff changes in the Loess Plateau |
title_short | Impact ways and their contributions to vegetation-induced runoff changes in the Loess Plateau |
title_sort | impact ways and their contributions to vegetation induced runoff changes in the loess plateau |
topic | Runoff change Budyko attribution analysis Vegetation variation The Loess Plateau |
url | http://www.sciencedirect.com/science/article/pii/S2214581823003178 |
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