Impact of climate change and vegetation greening on sediment transport in the Yarlung Tsangpo River

• Climate warming increases sediment load in the upper YTR by accelerating sediment mobilization in deglaciated areas. • Precipitation dominates the downstream sediment load through amplifying rainfall and hillslope erosion. • The increasing runoff and sediment load have crucial implications for sustainability of water resource management and riverine infrastructure. The Yarlung Tsangpo River (YTR), an essential headwater of the Tibetan Plateau, has experienced rapid warming and significant changes in sediment load over recent decades, threatening aquatic ecosystems, infrastructure integrity, and downstream water security. However, the relative and combined impacts of climate change, cryosphere degradation, and vegetation greening on sediment load remain insufficiently quantified, particularly across spatially heterogeneous cryosphere-fed river basins. Here, we integrate long-term (1981–2008/2009) in-situ hydrological observations with high-resolution meteorological and vegetation datasets to examine the sediment dynamics of the YTR in response to changing climate, cryospheric processes, and vegetation conditions. Our results reveal that sediment load has increased by 50–88 %, outpacing the 20–27 % rise in runoff during the study period. In the relatively cold and arid upstream region, sediment load is sensitive to both temperature (35 ± 2 %) and precipitation (45 ± 5 %), with warming-induced glacier retreat and permafrost thaw further amplifying sediment supply. In contrast, the relatively warm and humid downstream region is dominated by pluvial erosion associated with intensified rainfall (53 ± 3 %). These findings highlight pronounced spatial variations in sediment-climate-connectivity interactions and underscore their growing impacts on water quality, reservoir sedimentation, and hydropower efficiency. The pre-dam observational data presented here serve as a valuable baseline for future assessments of infrastructure impacts, offering critical support for hydropower planning, ecosystem protection, and adaptive sediment management under changing environmental conditions.

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Publication Details

Journal
CATENA
Published
2025-10-19
DOI
https://doi.org/10.1016/j.catena.2025.109557
Primary Topic
Cryospheric studies and observations
Type
article
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article

Impact of climate change and vegetation greening on sediment transport in the Yarlung Tsangpo River

Yi Zhao, Yiyi Li, Qiang Zhong, Yingchun Guo et al.
CATENA
Cryospheric studies and observations
article

Impact of climate change and vegetation greening on sediment transport in the Yarlung Tsangpo River

Yi Zhao, Yiyi Li, Qiang Zhong, Yingchun Guo, Peng Han, Yichu Wang, Liu Liu, Ting Zhang, Dongfeng Li, Shifeng Mao
article en

Abstract

• Climate warming increases sediment load in the upper YTR by accelerating sediment mobilization in deglaciated areas. • Precipitation dominates the downstream sediment load through amplifying rainfall and hillslope erosion. • The increasing runoff and sediment load have crucial implications for sustainability of water resource management and riverine infrastructure. The Yarlung Tsangpo River (YTR), an essential headwater of the Tibetan Plateau, has experienced rapid warming and significant changes in sediment load over recent decades, threatening aquatic ecosystems, infrastructure integrity, and downstream water security. However, the relative and combined impacts of climate change, cryosphere degradation, and vegetation greening on sediment load remain insufficiently quantified, particularly across spatially heterogeneous cryosphere-fed river basins. Here, we integrate long-term (1981–2008/2009) in-situ hydrological observations with high-resolution meteorological and vegetation datasets to examine the sediment dynamics of the YTR in response to changing climate, cryospheric processes, and vegetation conditions. Our results reveal that sediment load has increased by 50–88 %, outpacing the 20–27 % rise in runoff during the study period. In the relatively cold and arid upstream region, sediment load is sensitive to both temperature (35 ± 2 %) and precipitation (45 ± 5 %), with warming-induced glacier retreat and permafrost thaw further amplifying sediment supply. In contrast, the relatively warm and humid downstream region is dominated by pluvial erosion associated with intensified rainfall (53 ± 3 %). These findings highlight pronounced spatial variations in sediment-climate-connectivity interactions and underscore their growing impacts on water quality, reservoir sedimentation, and hydropower efficiency. The pre-dam observational data presented here serve as a valuable baseline for future assessments of infrastructure impacts, offering critical support for hydropower planning, ecosystem protection, and adaptive sediment management under changing environmental conditions.

CATENAVol. 261
Peking University (CN), Beijing Normal University (CN), Institute of Disaster Prevention (CN), China Agricultural University (CN)
Openalex Percentile: Top 65%
Cryospheric studies and observations
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