4.5 Article

Discharge Determines Avulsion Regime in Model Experiments With Vegetated and Unvegetated Deltas

Journal

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2021JF006225

Keywords

river delta; coastal processes; vegetation; water discharge; sediment discharge; channel dynamics

Funding

  1. National Science Foundation, Geomorphology and Land-Use Dynamics Program [1324114, 1530233]
  2. Division Of Earth Sciences
  3. Directorate For Geosciences [1324114, 1530233] Funding Source: National Science Foundation

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The dynamics and morphological evolution of deltas and their channel networks are influenced by water and sediment discharge, vegetation, and other factors. The study explores how water and sediment discharge affect delta evolution and how vegetation stabilizes the channel network. The findings provide insights into avulsion dynamics and the role of vegetation in channel stability under different discharge conditions.
The dynamics and morphological evolution of deltas and their channel networks involve interactions between many factors, including water and sediment discharge and cohesion from fine sediment and vegetation. These interactions are likely to affect how strongly vegetation influences deltas. Altering water or sediment discharge may affect channel mobility, magnitude of deposition and erosion events, and may result in the delta being less suitable for vegetation colonization. Using the numerical model DeltaRCM Vegetation, we explore how water and sediment discharge affects delta evolution and under which conditions vegetation exerts a stabilizing effect on the channel network. We propose new insights into delta evolution under different discharge conditions. First, we observe a regime shift in avulsion dynamics, driven by delta-scale water surface slopes, with increasing water discharge: from a few active channels undergoing occasional complete, global avulsions (with low discharge) to many active channels experiencing frequent partial, local avulsions (with high discharge). Second, with vegetation, increased sediment discharge results in more frequent switching of the dominant channels but also prevents vegetation from establishing in non-dominant channels, resulting in more frequent channel reoccupation and therefore greater stability in channel network planform. These insights have important implications for understanding the distribution of water, sediment, and nutrients on deltas in the face of future changes in climate and human modifications of fluxes of sediment and water to the coast, especially for restored or engineered deltas with controlled water or sediment discharges.

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