During the period from 2018 to 2023, the overall trend of the water load variation coefficient showed an increasing trend, indicating that, in recent years, the water intake in the LYR has gradually increased, as shown in Fig. 3 d.
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Response of sediment delivery ratio to water-sediment and riverbed boundary conditions during flood events in the lower yellow river since 2000.
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The G − A reach and A − L reach show a decreasing trend in river gradient related to aggradation during the non−flood season, as illustrated in Fig. 5 c and d.