Evolution and Attribution of Flood Volume in the Source Region of the Yellow River

Accurately understanding flood evolution and its attribution is crucial for watershed water resource management as well as disaster prevention and mitigation. The source region of the Yellow River (SRYR) has experienced several severe floods over the past few decades, but the driving factor influenc...

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Published in:Remote Sensing
Main Authors: Jie Wang, Donghui Shangguan, Yongjian Ding, Yaping Chang
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2025
Subjects:
Online Access:https://doi.org/10.3390/rs17081342
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author Jie Wang
Donghui Shangguan
Yongjian Ding
Yaping Chang
author_facet Jie Wang
Donghui Shangguan
Yongjian Ding
Yaping Chang
author_sort Jie Wang
collection MDPI Open Access Publishing
container_issue 8
container_start_page 1342
container_title Remote Sensing
container_volume 17
description Accurately understanding flood evolution and its attribution is crucial for watershed water resource management as well as disaster prevention and mitigation. The source region of the Yellow River (SRYR) has experienced several severe floods over the past few decades, but the driving factor influencing flood volume variation in the SRYR remains unclear. In this study, the Budyko framework was used to quantify the effects of climate change, vegetation growth, and permafrost degradation on flood volume variation in six basins of the SRYR. The results showed that the flood volume decreased before 2000 and increased after 2000, but the average value after 2000 remained lower than that before 2000. Flood volume is most sensitive to changes in precipitation, followed by changes in landscape in all basins. The decrease in flood volume was primarily influenced by changes in active layer thickness in permafrost-dominated basins, while it was mainly controlled by other landscape changes in non-permafrost-dominated basins. Meanwhile, the contributions of changes in potential evapotranspiration and water storage changes to the reduced flood volume were negative in all basins. Furthermore, the impact of vegetation growth on flood volume variation cannot be neglected due to its regulating role in the hydrological cycle. These findings can provide new insights into the evolution mechanism of floods in cryospheric basins and contribute to the development of strategies for flood control, disaster mitigation, and water resource management under a changing climate.
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spelling ftmdpi:oai:mdpi.com:/2072-4292/17/8/1342/ 2025-05-11T14:08:21+00:00 Evolution and Attribution of Flood Volume in the Source Region of the Yellow River Jie Wang Donghui Shangguan Yongjian Ding Yaping Chang agris 2025-04-09 application/pdf https://doi.org/10.3390/rs17081342 eng eng Multidisciplinary Digital Publishing Institute Remote Sensing in Geology, Geomorphology and Hydrology https://dx.doi.org/10.3390/rs17081342 https://creativecommons.org/licenses/by/4.0/ Remote Sensing Volume 17 Issue 8 Pages: 1342 flood volume climate change permafrost degradation vegetation growth source region of the Yellow River Text 2025 ftmdpi https://doi.org/10.3390/rs17081342 2025-04-15T00:02:26Z Accurately understanding flood evolution and its attribution is crucial for watershed water resource management as well as disaster prevention and mitigation. The source region of the Yellow River (SRYR) has experienced several severe floods over the past few decades, but the driving factor influencing flood volume variation in the SRYR remains unclear. In this study, the Budyko framework was used to quantify the effects of climate change, vegetation growth, and permafrost degradation on flood volume variation in six basins of the SRYR. The results showed that the flood volume decreased before 2000 and increased after 2000, but the average value after 2000 remained lower than that before 2000. Flood volume is most sensitive to changes in precipitation, followed by changes in landscape in all basins. The decrease in flood volume was primarily influenced by changes in active layer thickness in permafrost-dominated basins, while it was mainly controlled by other landscape changes in non-permafrost-dominated basins. Meanwhile, the contributions of changes in potential evapotranspiration and water storage changes to the reduced flood volume were negative in all basins. Furthermore, the impact of vegetation growth on flood volume variation cannot be neglected due to its regulating role in the hydrological cycle. These findings can provide new insights into the evolution mechanism of floods in cryospheric basins and contribute to the development of strategies for flood control, disaster mitigation, and water resource management under a changing climate. Text Active layer thickness permafrost MDPI Open Access Publishing Remote Sensing 17 8 1342
spellingShingle flood volume
climate change
permafrost degradation
vegetation growth
source region of the Yellow River
Jie Wang
Donghui Shangguan
Yongjian Ding
Yaping Chang
Evolution and Attribution of Flood Volume in the Source Region of the Yellow River
title Evolution and Attribution of Flood Volume in the Source Region of the Yellow River
title_full Evolution and Attribution of Flood Volume in the Source Region of the Yellow River
title_fullStr Evolution and Attribution of Flood Volume in the Source Region of the Yellow River
title_full_unstemmed Evolution and Attribution of Flood Volume in the Source Region of the Yellow River
title_short Evolution and Attribution of Flood Volume in the Source Region of the Yellow River
title_sort evolution and attribution of flood volume in the source region of the yellow river
topic flood volume
climate change
permafrost degradation
vegetation growth
source region of the Yellow River
topic_facet flood volume
climate change
permafrost degradation
vegetation growth
source region of the Yellow River
url https://doi.org/10.3390/rs17081342