Authors

Marc Simard, California Institute of Technology
Cathleen E. Jones, California Institute of Technology
Robert R. Twilley, Louisiana State University
Edward Castañeda-Moya, Florida International University
Sergio Fagherazzi, Boston University
Cédric G. Fichot, Boston University
Michael P. Lamb, Division of Geological and Planetary Sciences
Paola Passalacqua, Cockrell School of Engineering
Tamlin M. Pavelsky, The University of North Carolina at Chapel Hill
David R. Thompson, California Institute of Technology
Saoussen Belhadj-aissa, California Institute of Technology
Pradipta Biswas, Louisiana State University
Alexandra Christensen, California Institute of Technology
Luca Cortese, Boston University
Michael Denbina, California Institute of Technology
Carmine Donatelli, Boston University
Sarah Flores, California Institute of Technology
Andy Fontenot, Louisiana State University
Joshua P. Harringmeyer, Boston University
Daniel Jensen, California Institute of Technology
John Mallard, Cockrell School of Engineering
Justin Nghiem, Division of Geological and Planetary Sciences
Talib Oliver-Cabrera, California Institute of Technology
Ali Reza Payandeh, California Institute of Technology
Andre S. Rovai, Louisiana State University
Elena Solohin, Florida International University
Antoine Soloy, California Institute of Technology
Bhuvan Varugu, California Institute of Technology
Dongchen Wang, Division of Geological and Planetary Sciences
Kyle Wright, The University of Texas at Austin
Xiaohe Zhang, Boston University
Yang Zheng, California Institute of Technology

Document Type

Article

Publication Date

3-1-2026

Abstract

Coastal river deltas are highly dynamic regions with hydrological processes that vary on hourly, daily, and seasonal timescales. Soil formation in deltas relies on the balance between mineral sediment deposition, erosion, and organic matter production, which are intricately controlled by vegetation and hydrodynamic conditions. The spatial complexity and rapid variations in flow, particularly due to tides, present a major challenge to spaceborne remote sensing achieving the required spatial resolution and temporal sampling. Here, we present an airborne remote sensing and in situ framework that measures parameters that are critical to calibrate and validate hydrodynamic, sediment transport, morphodynamic, and ecogeomorphic models. We discuss the measurements and models within the context of the NASA Earth Venture-Suborbital Delta-X mission, which implemented the framework in two deltaic regions of the Mississippi River Delta with contrasting hydrological regimes, namely the Atchafalaya (i.e., active, river-dominated) and Terrebonne (inactive, river-abandoned) basins that are undergoing land gain and land loss, respectively. The Delta-X framework uses two airborne radar instruments to monitor hydrodynamic processes, measuring water surface level and slope within channels, and tide-induced water level change within wetlands. In addition, an airborne imaging spectrometer provides estimates of suspended sediment concentrations in open water as well as vegetation type and aboveground biomass. We also discuss how the data are used to calibrate and validate the models that estimate sediment deposition and organic soil production, which build land to offset subsidence and sea level rise.

Publication Source (Journal or Book title)

Remote Sensing of Environment

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