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This repository houses information related to the coastal vegetation group.

Contributors

Elena Bastianon, University of Hull
Isamar Cortes, Montclair State University
Elizabeth Davis, Virginia Institute of Marine Science, William & Mary
Kelly Sanks, Tulane University
Lexi Van Blunk, North Carolina State University

Introduction

Mangroves and salt marsh ecotone regions are migrating towards the poles due to climatic changes such as increasing temperatures and shifting salinity regimes. IMPLICATION OF CHANGE. In this analysis, we examine how dominant vegetation type (i.e., marsh or mangroves) influences delta evolution and sediment accretion over a 50 year time period.

Learning Objectives

Skills

Key Concepts

Acknowledgements

This material was enabled and encouraged by the contributors' participation in the Community Surface Dynamics Modeling System (CSDMS) Spring School in 2022. This work was presented during the 2022 CSDMS Annual Meeting.

References

Lauzon, R. & Murray, A. B. (2018). Comparing the cohesive effects of mud and vegetation on delta evolution. Geophysical Research Letters, 45(19), 10-437.
Liang, M.; Voller, V. R.; Paola, C. (2015). A reduced-complexity model for river delta formation; Part 1: Modeling deltas with channel dynamics. Earth Surface Dynamics, 3, 67–86. 10.5194/esurf-3-67-2015
Liang, M.; Geleynse, N.; Edmonds, D. A.; Passalacqua, P. (2015). A reduced-complexity model for river delta formation; Part 2: Assessment of the flow routing scheme. Earth Surface Dynamics, 3, 87–104. 10.5194/esurf-3-87-2015
Willemsen, Pim; Horstman, Erik; Borsje, B.W.; Friess, Daniel; Dohmen-Janssen, Marjolein (2016). Sensitivity of sediment trapping capacity of estuarine mangrove forests: Geomorphology. 273. 10.1016/j.geomorph.2016.07.038.