Experiment to explore the impact of flooding on delta surface processes. Two flooding states were imposed: high-intensity flooding, and low-intensity flooding. The system cycled between these states over the experimental runtime. Each flood regime was held constant for a set period to allow surface processes to equilibrate between each transition. Each transition in flooding took place over a planned duration. The water level rise in the basin and the integrated water and sediment flux were held constant over the experimental runtime.
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