Deltaic wetlands are uniquely vulnerable to sea level rise due to their coastal setting, low elevation gradient, and the high rate of subsidence in recently deposited sediments (Blum & Roberts, 2009;Giosan et al., 2014;Hoitink et al., 2020;Törnqvist et al., 2020). Many deltas host dense human populations that rely on vast expanses of wetlands for critical ecosystem services including protection from storms (e.g., Edmonds et al., 2020). Despite the vulnerability that is inherent in a delta setting, deltaic ecosystems are also uniquely able to adapt to sea level rise by making use of the riverine sediment transport system to locally increase elevation. A delta's distributary channels provide both the source of sediment and the means for delivering sediment to the locations where it can be most useful for land building. In many deltas the connections between distributary channels and the delta plain have been restricted (e.g., Esposito et al., 2020), and land use managers are working to plan diversions of water and sediment that will leverage delta sediment transport processes to deliver sediment to vulnerable or valuable wetlands (