4.7 Article

Dynamics of sediment transport in the Yangtze River and their key drivers

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SCIENCE OF THE TOTAL ENVIRONMENT
卷 862, 期 -, 页码 -

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ELSEVIER
DOI: 10.1016/j.scitotenv.2022.160688

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Sediment load change; Climate change; Distributed hydrological model; Yangtze River

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Understanding the dynamics of sediment transport and their underlying driving mechanisms is critical to sustainable river basin management. However, there is a lack of quantification of various drivers of sediment load change, and the impact of climate change on sediment transport under different global warming scenarios is not well understood.
Understanding the dynamics of sediment transport and their underlying driving mechanisms is critical to developing strategic plans for sustainable river basin management. However, the quantification of various drivers (e.g., dam construction, soil and water conservation measures) of sediment load change remains scarce, and the projections of sediment transport under the 1.5 degrees C and 2.0 degrees C global warming scenarios are not well understood. Here we quantify the sediment load dynamics in the Yangtze River and also estimate the relative contributions of climate change and human activities to these changes using the Soil and Water Assessment Tool (SWAT) hydrologic model and statistical methods. Results show that the sediment load exhibited a significant decreasing trend at most stations in the Yangtze River, with breakpoints occurring around 1993 and 2003. The study period of 1972-2016 can be split into three subperiods: 1972-1992 (P1), 1993-2003 (P2), and 2004-2016 (P3). From P1 to P3, 95.6 % of the decline can be attributed to climate change, the remainder resulting from the construction of dams and reservoirs (3.6 %) and improved soil and water conservation (0.8 %). Specifically, human activities contributed similar to 67.96 % to sediment changes during the period P1-P2, whereas climatic change contributed similar to 81.76 % during the period P2-P3. The sediment load significantly increased in the RCP 2.6 (slope = 0.87 Mt center dot yr-1, P < 0.01) and RCP 4.5 (slope = 0.84 Mt center dot yr-1, P < 0.05) under the global warming of 1.5 degrees C and 2.0 degrees C towards the entire Yangtze River. Compared with the 2.0 degrees C (2040-2059) global warming scenario, the mean annual sediment load in the 1.5 degrees C (2020-2039) global warming scenario is smaller by 17.88 Mt. Our investigation found that climate variations will provide a more remarkable contribution to sediment load dynamics in the Yangtze River in the future than the historical average due to the effectiveness of reservoirs

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