Coastal zones are inhabited by three-quarters of the global population and contribute to more than half of the global gross domestic product (GDP) despite accounting for only 5% of the Earth's land mass. Within coastal zones, river deltas are alluvial plains formed by the deposition of sediment and often occur where inland water flow leaves river estuaries and meets salty, stagnant ocean water. River deltas are home to more than half-a-billion people and are a crux of human civilization. The morphology of river deltas highly depends on the oceanographic forces of tides and waves and is also regularly reshaped by deltaic sediment cycling, which can be influenced by anthropogenic activities, such as damming and deforestation, resulting in the gain or loss of land area (Nienhuis et al., 2020;Syvitski et al., 2009). Quantifying the individual importance of tides, waves, and fluvial sediment supply in river delta formation is critical for policymakers to understand potential threats to deltas and develop adaptation strategies.As one of the largest deltas in Asia, the Pearl River Delta (see Figure 1a) is known for its high population density and economic level. The GDP of the Pearl River Delta reached 1,084.5 billion USD by 2017, accounting for nearly 9.1% of the GDP of mainland China (Statistics Bureau of Guangdong Province, 2019).